Geological exploration method and device based on material intrinsic subatomic wave radiation characteristics

Abstract

The embodiment of the invention provides a geological exploration method and device based on material intrinsic subatomic wave radiation characteristics, and the method comprises the steps: carrying out the remote sensing satellite data obtaining operation through the specific range of a target mining area, a set scale, a set shooting angle, a set time period, and a set wave band, and determining a remote sensing satellite original negative film of a corresponding exploration area; performing radiation operation on the original negative film according to a preset subatomic field generator, performing image enhancement processing on the target substance radiation image according to a nonlinear algorithm, and determining a corresponding target substance digital map; the method comprises the following steps: determining three corresponding directions according to a digital map, respectively determining three corresponding digital images according to the three directions, carrying out target substance inversion calculation and target substance model establishment operation according to the three digital images, determining a corresponding target substance mathematical model, and realizing target substance visualization. According to the method, the subatomic radiation of the earth crust mineral elements can be captured based on the satellite, mineral detection and visualization are carried out by utilizing the subatomic characteristics, and the efficiency and accuracy of geological exploration are improved.

Description

Technical Field

[0001] The present application relates to the field of data processing, and in particular to a geological exploration method and device based on the radiation characteristics of intrinsic subatomic waves of matter. Background Art

[0002] The existing exploration methods for underground rocks and minerals (deposits) mainly include geological exploration, geophysical exploration, geochemical exploration, drilling engineering and other methods. These methods have their own characteristics and are suitable for different exploration purposes and geological conditions.

[0003] Geological exploration is to make geological maps of a certain scale through systematic geological observation and measurement to identify the geological structural characteristics of the work area and the geological conditions for the formation and occurrence of minerals. However, with the development of society, the demand for mineral resources is increasing. The existing shallow mineral resource reserves can no longer meet the needs of social development. Mineral resource exploration urgently needs to advance into the deep, which limits the development of this method.

[0004] Geophysical exploration is a method of finding and exploring mineral deposits by using the differences in the physical characteristics of geological bodies. It is a physical exploration method that uses instruments and equipment to observe gravity, magnetic, electric and electromagnetic field data on the surface to analyze the morphology of deep geological bodies. However, the biggest drawback of this method is that the method theory itself is a multi-solution equation, that is, the results of the method detection have multi-solutions. For the current deeper prospecting, this method is limited in its ability.

[0005] Geochemical exploration starts with studying the distribution of various elements in the earth's crust and the laws of migration and enrichment in various geological processes. Through systematic sampling and analysis, the dispersion halos formed when various mineralizing elements are enriched are discovered, thereby achieving the purpose of prospecting. However, geochemical exploration also has obvious shortcomings. Elements are enriched in the earth's crust to form ore bodies. With millions of years of geological movement and groundwater migration, element chemical anomalies will also migrate, resulting in a large positional deviation between the geochemical anomalies we have identified and the actual ore body location.

[0006] Other technical methods, such as remote sensing, are difficult to interpret, which limits their application in mineral exploration.

[0007] In summary, there are many methods for geological exploration, but each has its own shortcomings. The exploration of underground rocks and minerals (ore deposits) is multi-solution, the accuracy is not high, and it cannot adapt to the complex changes of ore deposits and underground minerals over thousands of years. Therefore, it is urgent to propose a new geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter to overcome the multi-solution of mineral exploration and improve the accuracy and efficiency of underground mineral exploration. Summary of the invention

[0008] In response to the problems in the prior art, the present application provides a geological exploration method and device based on the intrinsic subatomic wave radiation characteristics of matter, which can capture the subatomic radiation of crustal mineral elements based on satellites, and use subatomic characteristics to perform mineral detection and visualization to improve the efficiency and accuracy of geological exploration.

[0009] In order to solve at least one of the above problems, the present application provides the following technical solutions:

[0010] In a first aspect, the present application provides a geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter, comprising:

[0011] Determine the specific scope of the target mining area, perform remote sensing satellite data acquisition operations according to the specific scope, set scale, set shooting angle, set time period and set band, determine the corresponding remote sensing satellite digital image of the exploration area, perform special mathematical calculation processing on the remote sensing satellite digital image of the exploration area, and perform laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing to determine the corresponding remote sensing satellite original negative of the exploration area;

[0012] Performing radiation operation on the original film according to a preset subatomic field generator to determine a corresponding radiation image of the target substance, performing image enhancement processing on the radiation image of the target substance according to a nonlinear algorithm to determine a corresponding enhanced radiation image, and performing digitization operation on the enhanced radiation image according to preset geographic coordinates and a preset vector algorithm to determine a corresponding digital map of the target substance;

[0013] Determine the corresponding three directions according to the digital map, perform radiation operations on the original film according to the three directions respectively, determine the corresponding three digital images, perform target material inversion calculation and target material model establishment operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization.

[0014] Furthermore, the remote sensing satellite data acquisition operation is performed according to the specific range, the set scale, the set shooting angle, the set time period and the set band to determine the corresponding remote sensing satellite digital image of the survey area, including:

[0015] Selecting a scale of the remote sensing satellite image according to the specific range to determine a corresponding set scale, wherein the set scale includes at least one of a large scale, a medium scale, and a small scale;

[0016] Selecting a shooting angle of the remote sensing satellite image according to the specific range to determine a corresponding set shooting angle, wherein the selection range of the set shooting angle is 0-180°;

[0017] Selecting a time period of the remote sensing satellite image according to the specific range to determine a corresponding set time period, wherein the time interval of the set time period is 30 minutes;

[0018] Selecting a band of the remote sensing satellite image according to the specific range to determine a corresponding set band, wherein the set band includes at least one of radio frequency, optical, short-wave infrared, long-wave infrared and ultraviolet;

[0019] The remote sensing satellite data acquisition operation is performed according to the set scale, set shooting angle, set time period and set band to determine the corresponding remote sensing satellite digital image of the survey area.

[0020] Furthermore, the special mathematical calculation processing is performed on the remote sensing satellite digital image of the survey area, and the digital image obtained after the special mathematical calculation processing is laser printed and calibrated to determine the corresponding remote sensing satellite original negative of the survey area, including:

[0021] Performing Fourier transform operation and image fusion operation on the remote sensing satellite digital image of the survey area to determine the corresponding high-precision remote sensing satellite digital image;

[0022] Laser printing and calibration operations are performed on the high-precision remote sensing satellite digital image to determine the corresponding remote sensing satellite original negative film of the survey area.

[0023] Furthermore, the radiation operation is performed on the original film according to the preset subatomic field generator to determine the corresponding radiation image of the target substance, including:

[0024] Performing a radiation operation on the original film according to a subatomic field emitted by a preset subatomic field generator having the same radiation frequency as that of the target material;

[0025] According to the radiation resonance of the target substance obtained after the radiation operation is received by the preset photosensitive film, a corresponding radiation image of the target substance is determined.

[0026] Further, performing image enhancement processing on the radiation image of the target material according to a nonlinear algorithm to determine a corresponding enhanced radiation image includes:

[0027] Performing a denoising operation on the target material radiation image according to a nonlinear filtering algorithm to determine a corresponding first material radiation image;

[0028] An image feature extraction operation is performed on the radiation image of the first material according to a nonlinear image processing algorithm to determine a corresponding enhanced radiation image.

[0029] Furthermore, the enhanced radiation image is digitized according to preset geographic coordinates and a preset vector algorithm to determine a corresponding digital map of the target material;

[0030] Performing a plane position calibration operation on the enhanced radiation image according to preset geographic coordinates;

[0031] A vectorization operation is performed on the image after the plane position calibration operation according to a preset vector algorithm to determine a corresponding vectorized radiation image, and a digitization operation is performed on the vectorized radiation image to determine a corresponding digital map of the target material.

[0032] Further, determining the corresponding three directions according to the digital map includes:

[0033] Determining a corresponding vertical direction according to the digital map;

[0034] Determine a corresponding contour anomaly map according to the coordinates in the digital map, perform a profile cutting operation on the contour anomaly map, and determine the inclination and dip angle of the corresponding target material;

[0035] The corresponding vertical tilt angle direction and parallel tilt angle direction are determined according to the tilt angle.

[0036] Furthermore, the radiation operation is performed on the original film according to the three directions respectively to determine the corresponding three digital images, including:

[0037] Performing a radiation operation on the original film according to the vertical direction to determine a corresponding vertical radiation image;

[0038] Performing a radiation operation on the original film according to the vertical inclination direction to determine a corresponding vertical inclination radiation image;

[0039] The original film is subjected to a radiation operation according to the parallel tilt angle direction to determine a corresponding parallel tilt angle radiation image.

[0040] Furthermore, the target material inversion calculation and target material model establishment operations are performed according to the three digital images to determine the corresponding target material mathematical model, including:

[0041] Determine the corresponding target material burial depth according to the vertical inclination radiation image and the vertical radiation image;

[0042] Determine the corresponding target material thickness according to the parallel tilt angle radiation image;

[0043] A corresponding mathematical model of the target material is determined according to the buried depth of the target material and the thickness of the target material.

[0044] In a second aspect, the present application provides a geological exploration device based on the intrinsic subatomic wave radiation characteristics of matter, comprising:

[0045] The original film customization module is used to determine the specific scope of the target mining area, perform remote sensing satellite data acquisition operations according to the specific scope, set scale, set shooting angle, set time period and set band, determine the corresponding remote sensing satellite digital image of the exploration area, perform special mathematical calculation processing on the remote sensing satellite digital image of the exploration area, and perform laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing to determine the corresponding remote sensing satellite original film of the exploration area, wherein the historical form usage data includes at least one of historical form performance data and historical form structure change data;

[0046] A radiation image extraction module is used to perform a radiation operation on the original film according to a preset subatomic field generator to determine a corresponding target material radiation image, perform image enhancement processing on the target material radiation image according to a nonlinear algorithm to determine a corresponding enhanced radiation image, and perform a digitization operation on the enhanced radiation image according to preset geographic coordinates and a preset vector algorithm to determine a corresponding target material digital map;

[0047] The mineral mathematical model building module is used to determine the corresponding three directions according to the digital map, perform radiation operations on the original film according to the three directions respectively, determine the corresponding three digital images, perform target material inversion calculation and target material model building operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization.

[0048] In a third aspect, the present application provides an electronic device comprising a memory, a processor, and a computer program stored in the memory and executable on the processor, wherein when the processor executes the program, the steps of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter are implemented.

[0049] In a fourth aspect, the present application provides a computer-readable storage medium having a computer program stored thereon, which, when executed by a processor, implements the steps of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter.

[0050] In a fifth aspect, the present application provides a computer program product, including a computer program / instruction, which, when executed by a processor, implements the steps of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter.

[0051] It can be seen from the above technical scheme that the present application provides a geological exploration method and device based on the intrinsic subatomic wave radiation characteristics of matter, which performs remote sensing satellite data acquisition operations through the specific scope of the target mining area, set scale, set shooting angle, set time period and set band, and determines the original remote sensing satellite film of the corresponding exploration area; performs radiation operations on the original film according to a preset subatomic field generator, and performs image enhancement processing on the radiation image of the target material according to a nonlinear algorithm to determine the corresponding digital map of the target material; determines the corresponding three directions according to the digital map, determines the corresponding three digital images according to the three directions respectively, performs target material inversion calculation and target material model establishment operations according to the three digital images, determines the corresponding mathematical model of the target material, and realizes visualization of the target material, thereby being able to capture the subatomic radiation of crustal mineral elements based on satellites, and use subatomic characteristics to perform mineral detection and visualization, thereby improving the efficiency and accuracy of geological exploration. BRIEF DESCRIPTION OF THE DRAWINGS

[0052] In order to more clearly illustrate the embodiments of the present application or the technical solutions in the prior art, the drawings required for use in the embodiments or the description of the prior art will be briefly introduced below. Obviously, the drawings described below are some embodiments of the present application. For ordinary technicians in this field, other drawings can be obtained based on these drawings without paying any creative work.

[0053] Figure 1 This is one of the flow diagrams of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the embodiment of the present application;

[0054] Figure 2 This is the second flow chart of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the embodiment of the present application;

[0055] Figure 3 This is the third flow chart of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the embodiment of the present application;

[0056] Figure 4 This is a fourth flow chart of a geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in an embodiment of the present application;

[0057] Figure 5 This is the fifth flow chart of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the embodiment of the present application;

[0058] Figure 6 This is the sixth flow chart of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the embodiment of the present application;

[0059] Figure 7This is the seventh flow chart of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the embodiment of the present application;

[0060] Figure 8 This is the eighth flow chart of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the embodiment of the present application;

[0061] Fig. 9 This is a ninth flow chart of a geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in an embodiment of the present application;

[0062] Fig.10 It is a structural diagram of a geological exploration device based on the radiation characteristics of intrinsic subatomic waves of matter in an embodiment of the present application;

[0063] Fig.11 It is a schematic diagram of the structure of an electronic device in an embodiment of the present application.

[0064] Reference numerals:

[0065] Electronic device 9600, central processing unit 9100, memory 9140, communication module 9110, input unit 9120, audio processor 9130, display 9160, power supply 9170, buffer memory 9141, application / function storage unit 9142, data storage unit 9143, driver program storage unit 9144, antenna 9111, speaker 9131, microphone 9132. DETAILED DESCRIPTION

[0066] In order to make the purpose, technical solution and advantages of the embodiments of the present application clearer, the technical solution in the embodiments of the present application will be clearly and completely described below in conjunction with the drawings in the embodiments of the present application. Obviously, the described embodiments are part of the embodiments of the present application, not all of the embodiments. Based on the embodiments in the present application, all other embodiments obtained by ordinary technicians in this field without creative work are within the scope of protection of this application.

[0067] The acquisition, storage, use, and processing of data in the technical solution of this application comply with the relevant provisions of national laws and regulations.

[0068] Considering that there are many methods for geological exploration at present, but each has its own shortcomings, the exploration of underground rocks and minerals (ore deposits) has multiple solutions, low accuracy, and cannot adapt to the complex changes of ore deposits and underground minerals for thousands of years. The present application provides a geological exploration method and device based on the intrinsic subatomic wave radiation characteristics of matter, through the specific scope of the target mining area, set scale, set shooting angle, set time period and set band to perform remote sensing satellite data acquisition operation, determine the original film of the remote sensing satellite in the corresponding exploration area; perform radiation operation on the original film according to the preset subatomic field generator, perform image enhancement processing on the radiation image of the target material according to the nonlinear algorithm, and determine the corresponding target material digital map; determine the corresponding three directions according to the digital map, determine the corresponding three digital images according to the three directions, perform target material inversion calculation and target material model establishment operation according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization, thereby being able to capture the subatomic radiation of crustal mineral elements based on satellites, use subatomic characteristics to perform mineral detection and visualization, and improve the efficiency and accuracy of geological exploration.

[0069] In order to capture the subatomic radiation of crustal mineral elements based on satellites, use subatomic properties to detect and visualize minerals, and improve the efficiency and accuracy of geological exploration, this application provides an embodiment of a geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter, see Figure 1 The geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter specifically includes the following contents:

[0070] Step S101: determining the specific scope of the target mining area, performing remote sensing satellite data acquisition operations according to the specific scope, setting the scale, setting the shooting angle, setting the time period and setting the band, determining the corresponding remote sensing satellite digital image of the exploration area, performing special mathematical calculation processing on the remote sensing satellite digital image of the exploration area, and performing laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing, and determining the corresponding remote sensing satellite original negative of the exploration area;

[0071] Optionally, in this embodiment, the purpose of this step is to pre-process the remote sensing satellite data to obtain remote sensing satellite negatives that can be further processed with special lasers later.

[0072] Optionally, in this embodiment, the specific scope of the target mining area is determined, and remote sensing satellite data acquisition operations are performed based on the specific scope, set scale, set shooting angle, set time period and set band to determine the corresponding remote sensing satellite digital image of the exploration area.

[0073] Specifically, the specific scope of the target mining area requires the specific geographical scope and location of the exploration work to be clarified, including longitude and latitude coordinates and the approximate area scope.

[0074] Specifically, remote sensing satellite data acquisition operations should clarify the type, resolution, band, time resolution and other specific requirements of the required satellite data according to the purpose of the survey. Satellites that can provide the required scale, shooting angle, time resolution and band are selected according to the needs. This may involve high-resolution commercial satellites (such as GeoEye and WorldView series), scientific research satellites (such as Landsat and Sentinel series) or satellites for specific missions.

[0075] Specifically, set the scale and customize satellite images of different scales according to the survey needs. This may involve extracting and synthesizing images of different scales from high-resolution satellite data. Use professional software (such as ERDAS IMAGINE, ArcGIS, etc.) to scale, crop and splice images to meet the needs of different scales.

[0076] It is understandable that large-scale satellite images: small range, detailed content, suitable for precise measurement and detailed analysis. In mineral exploration, large-scale satellite images can clearly show the topography, geological structure and other detailed information of the mining area, which is helpful to find direct prospecting signs such as ore outcrops, mineralized alteration zones, etc.

[0077] Medium-scale satellite images: between large-scale and small-scale images, suitable for medium-scale regional surveys. In exploration work, medium-scale satellite images can provide more comprehensive regional geological background information, which helps to understand the structural framework and magmatic rock distribution of the mining area.

[0078] Small-scale satellite images: They show a wide range and a rough outline of the content, and are used to provide an overview of geographic information. Small-scale satellite images can show the geological structure and geomorphic features of the entire exploration area or even a larger area, which helps to grasp the geological background and prospecting direction of the mining area from a macro perspective.

[0079] Specifically, the shooting angle is set to take a satellite image every 3° within the range of 0-180°, ensuring that the satellite can adjust its shooting angle to cover the entire range. Considering the limitations of satellite orbit and attitude control, multiple passes or combining data from multiple satellites may be required to meet this requirement.

[0080] It is understandable that low-angle shooting makes the subject appear taller and more magnificent, increasing the visual impact. In mineral exploration, low-angle satellite images can highlight the height difference of the mining area and enhance the understanding of the topographic features.

[0081] High-angle shooting: Show the overall view and details of the scene, and increase the layering of the picture. Satellite images shot at high angles can fully display the layout and geological structure characteristics of the mining area, which helps to understand the overall geological conditions of the mining area.

[0082] Multi-angle shooting: By shooting at different angles, you can obtain multi-perspective information of the mining area, which helps to more comprehensively understand the geological characteristics and ore body morphology of the mining area. This is of great significance for the three-dimensional modeling of mineral deposits and the analysis of ore body morphology.

[0083] Specifically, set a time period and customize a satellite image every 30 minutes for 24 hours a day. This requires the satellite to have a high-frequency revisit capability or to use multiple satellites for collaborative observation. Ensure that the satellite can take stable images within the specified time period and record the exact time of each shot.

[0084] It is understandable that satellite images of different time periods can have the following observation functions:

[0085] Time series analysis can analyze the dynamic changes of mining areas by acquiring satellite images of different time periods. For example, in mineral exploration, the changes in vegetation coverage and surface water systems in mining areas can be analyzed to infer the geological effects and mineralization processes in mining areas.

[0086] Environmental change monitoring: Satellite images taken at different time periods can also be used to monitor environmental changes in mining areas, such as soil erosion, geological disasters, etc. This is of great significance for assessing environmental risks in mining areas and protecting the ecological environment.

[0087] Specifically, set the bands and customize satellite images in five bands: radio frequency, optical, short-wave infrared, long-wave infrared, and ultraviolet. This requires the satellite to have multi-spectral or hyperspectral imaging capabilities. According to the satellite's band coverage, select the band closest to the requirements for data collection.

[0088] It is understandable that the optical band is mainly used to obtain visible light and infrared band information in the mining area, reflecting the surface coverage and vegetation growth in the mining area. This is of great significance for understanding the natural environment and human activities in the mining area.

[0089] Short-wave infrared band: sensitive to the specific absorption characteristics of minerals, often used for mineral identification and lithology classification. In mineral exploration, short-wave infrared satellite images can reveal the absorption spectrum characteristics of minerals and help discover mineralized alteration zones and ore body outcrops.

[0090] Long-wave infrared band: Mainly used to monitor the surface temperature distribution and heat transfer process. In mineral exploration, long-wave infrared band satellite images can be used to study geothermal anomalies and underground hydrothermal activities in mining areas, providing clues for finding hydrothermal deposits.

[0091] Radio frequency and ultraviolet bands: Although not commonly used in conventional satellite remote sensing in mineral exploration, they have special application value under specific conditions (such as detecting underground pipelines, monitoring atmospheric composition, etc.).

[0092] In summary, satellite images of different scales, shooting angles, time periods, and bands have their own characteristics and functions in remote sensing exploration and monitoring. Together, they provide rich and comprehensive information support for mineral exploration and research in other fields.

[0093] Optionally, in this embodiment, special mathematical calculation processing is performed on the remote sensing satellite digital image of the exploration area, and the digital image obtained after the special mathematical calculation processing is laser printed and calibrated to determine the corresponding remote sensing satellite original film of the exploration area.

[0094] Optionally, in this embodiment, the special mathematical processing includes:

[0095] 1. Noise reduction: Periodic noise will overlap on the source image to form a series of peaks or bright spots, which can be eliminated by bandpass or slot filtering methods; spike noise can be filtered by Fourier transform.

[0096] 2. Eliminate bad lines and stripes: To eliminate bad lines and stripes in remote sensing images, Fourier transform and low-pass filtering are generally used to eliminate them.

[0097] 3. Thin cloud processing: Thin clouds appearing in remote sensing images due to weather reasons are weakened.

[0098] 4. Shadow processing: Due to the altitude of the sun, the mountain shadows that appear in the remote sensing image can be eliminated by using the ratio method.

[0099] 5. Geometric correction: To make the remote sensing images accurately positioned, they must be geometrically corrected before use. The method is to use the existing accurate geographic coordinate information and projection information to correct the original remote sensing images so that they have accurate geographic coordinate information. In areas with large terrain fluctuations, those orthorectification must also be performed. The method is to use the existing geographic reference data (topographic maps, control points, etc.) and digital elevation model data (DEM) to correct the original remote sensing images to eliminate or reduce the image deformation caused by the terrain fluctuations.

[0100] 6. Image enhancement: In order to make the ground object information contained in the remote sensing image more readable, the remote sensing image needs to be enhanced. The histogram transformation is used to count the number of pixels of each brightness in the image. The random distribution of pixel brightness should be normally distributed. The non-normal distribution of the histogram indicates that the image brightness distribution is too bright, too dark, or the brightness is too concentrated. The image contrast is small. The histogram needs to be adjusted to a normal distribution to improve the image quality.

[0101] 7. Image fusion: Different remote sensing data have different spatial resolutions, populated resolutions and temporal resolutions. Fusion of multi-source remote sensing data in a unified coordinate system and use of certain algorithms to generate a set of synthetic images can make up for the lack of information in a single image, expand the application scope of each information, and improve the accuracy of remote sensing image analysis.

[0102] It is understandable that the purpose of special mathematical processing is to make the remote sensing satellite digital images obtained more accurate while ensuring that more information can be extracted.

[0103] Step S102: performing radiation operation on the original film according to a preset subatomic field generator to determine a corresponding target material radiation image, performing image enhancement processing on the target material radiation image according to a nonlinear algorithm to determine a corresponding enhanced radiation image, performing digitization operation on the enhanced radiation image according to preset geographic coordinates and a preset vector algorithm to determine a corresponding target material digital map;

[0104] Optionally, in this embodiment, the purpose of this step is to perform subatomic field radiation on the original film obtained above, extract the radiation image of the target substance, and provide a basis for subsequent visualization of the target substance.

[0105] Optionally, in this embodiment, the original film is irradiated according to a preset subatomic field generator to determine a corresponding radiation image of the target substance.

[0106] Specifically, this step is carried out in a radioactive laboratory. The principle of radiation resonance is that when the leptons in a material body (such as rocks, ores, minerals, etc.) encounter energy fluctuations to form resonance conditions, they will show an energy difference response, thereby radiating a lepton field of a specific frequency. This radiation information can be captured and recorded by remote sensing equipment such as remote sensing satellites. The lepton field can absorb and re-emit radiation energy under the irradiation of a radiation source of a specific wavelength.

[0107] Since the subatomic field vibration frequencies of different substances are different, when extracting the subatomic resonance field, the vibration frequency of the subatomic field generator is selected according to the vibration frequency of the target substance in the vibration frequency spectrum of different substances, and the remote sensing satellite images are radiated to obtain the subatomic distributed radiation resonance field.

[0108] Next, the subatomic distributed radiation resonance field is projected onto the subatomic filter, and the radiation resonance of the target substance is accurately extracted through the filter and the gel of the substance to be collected arranged on the filter.

[0109] Subatomic filters can selectively filter radiation signals of specific wavelengths or energies, thereby extracting lepton radiation characteristics associated with target materials (such as ore bodies). This enables target signals to be more clearly identified against a complex background. In the process of data visualization, subatomic filters can help generate clearer and more informative radiation images, allowing researchers to more intuitively understand the distribution and characteristics of ore bodies.

[0110] The gel of the substance to be collected can effectively concentrate the minerals or compounds in the target sample, which is convenient for subsequent analysis, especially the extraction of trace elements. It focuses on sample processing and the improvement of detection sensitivity, and is used in combination with spectral analysis, chromatographic analysis and other technologies to improve analysis efficiency and accuracy.

[0111] Photographic film responds to radiation energy. By irradiating the target material with radiation resonance, the film can record these radiation signals. The material selection and processing of the film make it sensitive to slight changes in radiation.

[0112] During the experiment, a preset radiation source (such as a laser or other high-energy radiation source) will irradiate the photographic film. The purpose of this process is to enhance the signal and make the radiation characteristics of the target material more obvious. Through appropriate irradiation methods, changes in radiation flux can be effectively recorded.

[0113] When the photographic film receives the radiation signal, the radiation resonance forms corresponding images on the film. These images reflect the radiation characteristics of the target material, including radiation intensity and distribution pattern.

[0114] Optionally, the entire radioactivity test is conducted at three levels:

[0115] The original negative of the satellite image is placed on the top layer, and the satellite image on the top layer is vertically radiated by an external subatomic field generator;

[0116] The subatomic filter is placed in the middle layer to receive the resonance field of the top layer, and the accuracy of the target resonance field is improved through the filter and the gel of the substance to be collected;

[0117] The photosensitive film is placed at the bottom layer, and by arranging a radiation source at the bottom of the photosensitive film, the resonance field can be effectively imaged.

[0118] Preferably, the photosensitive film may be an X-ray film, and the radiation source below the photosensitive film may be an ultraviolet radiation source.

[0119] It can be understood that through the above steps, the original film is successfully irradiated by the atomic field generator to form a subatomic field resonance of the target substance, and the resonance field is received by the photosensitive film to form a radiation image of the target substance on the film.

[0120] Optionally, in this embodiment, image enhancement processing is performed on the radiation image of the target material according to a nonlinear algorithm to determine a corresponding enhanced radiation image.

[0121] Specifically, the nonlinear algorithm is a nonlinear image processing method, which refers to processing the image by using nonlinear mathematical operations and algorithms to improve the quality visualization effect of the image.

[0122] More specifically, nonlinear processing includes the following key links:

[0123] Image brightness and contrast adjustment: Through nonlinear transformation, the brightness and contrast of the image are optimized to make the image with abnormal radiation intensity distribution more clearly visible.

[0124] Noise Removal: Apply nonlinear filtering technology to remove noise from images and improve the overall image quality.

[0125] Feature description: Use nonlinear image processing technology to perform image edge detection, image segmentation, image enhancement and image compression to better describe the features and structures in the image and improve the visual effect.

[0126] This step lays a solid foundation for subsequent digital map drawing and mathematical model establishment, and can be said to be a key step in the visualization method.

[0127] Optionally, in this embodiment, the enhanced radiation image is digitized according to preset geographic coordinates and a preset vector algorithm to determine a corresponding digital map of the target material.

[0128] Specifically, the GIS geographic information system program is used to perform plane position calibration on the image after nonlinear processing. This process ensures that the extracted radiation intensity image corresponds to the geographic coordinate system and ensures the spatial position of the data is accurate. Through position calibration, the radiation anomaly phenomenon can be correctly located in the actual geographical environment, thereby providing a reliable geographical background for subsequent analysis.

[0129] Specifically, the geoscientific vectorization program is used to vectorize the images after nonlinear processing and calibration. The vectorization process converts the raster image (pixel-based) into vector data (points, lines, and surfaces), making the data more flexible and accurate in display and analysis. Vector data allows for more complex geological analysis and modeling, for example, it is easier to perform spatial analysis and overlay analysis, which improves the usability of the data.

[0130] It is understood that vector data is a representation of geographic information using points, lines, and surfaces. For example, in mineral exploration, the radiation anomaly area of ​​a mining area can be represented by a polygon, and the boundary of this polygon is connected by multiple points (coordinates). Vector data usually has a higher accuracy because it uses coordinates to accurately locate specific geographic features.

[0131] Specifically, relevant data is extracted from the vectorized image, including radiation flux density value, abnormal distribution area, abnormal position coordinates and other information.

[0132] The abnormal radiation range is divided according to the radiation flux density value, and the extracted range-related data is converted into digital format for storage and analysis by the computer system. These data are usually saved in the form of tables or databases. Using the GIS geographic information system, the digitized data is drawn into a digital map to show the spatial distribution of the radiation flux density.

[0133] It can be understood that the above steps obtain a digital map drawn according to the radiation flux density, which is computable and the coordinates are calibrated with the geographic location coordinates. The mathematical model calculation and visualization of the target ore body can be carried out through the radiation flux density anomaly.

[0134] Step S103: Determine three corresponding directions according to the digital map, perform radiation operations on the original film according to the three directions respectively, determine three corresponding digital images, perform target material inversion calculation and target material model establishment operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization.

[0135] Optionally, in this embodiment, the corresponding three directions are determined according to the digital map.

[0136] Specifically, the digital map is formed by the subatomic generator radiating vertically to the original film, and the vertical direction is the first direction;

[0137] Connect the numbers with the same radiation energy image in this digital map to form the corresponding target mineral radiation contour anomaly map. In the anomaly map, perform profile cutting on the peak anomaly to restore the dip and inclination of the target mineral. Draw the corresponding tangent to the inclination, and the direction of the tangent is the direction of the inclination. At this time, determine the direction along the inclination as the second direction, and the direction perpendicular to the inclination as the third direction.

[0138] Optionally, in this embodiment, radiation operations are performed on the original film according to the three directions respectively to determine three corresponding digital images.

[0139] Specifically, after obtaining the above three directions, the original film is radiated from the above three directions respectively through a subatomic generator to obtain three corresponding radiation images, among which the image radiated from the vertical direction is the vertical radiation image A, that is, the radiation image of the target material obtained in step S102; the image obtained by radiation from the vertical inclination direction is the vertical inclination radiation image B; the image obtained by radiation from the parallel inclination direction is the parallel inclination radiation image C.

[0140] It can be understood that the images radiated from the above three directions appear as three ellipses of different sizes on the plane. At the same time, the above image digitization process is repeated. After the coordinates of the elliptical image are calibrated and vectorized and digitized, the target material can be inverted and calculated through the coordinate points in the ellipse, a mathematical model of the target material can be established, and the target material can be visualized.

[0141] Optionally, in this embodiment, target material inversion calculation and target material model establishment operations are performed based on the three digital images to determine the corresponding target material mathematical model.

[0142] Specifically, the target material inversion calculation steps are as follows:

[0143] The left vertex A1, the right vertex A2 and the center point O1 of the vertical radiation image A of the target material;

[0144] The left vertex B1, the right vertex B2 and the center point O2 of the vertical inclination radiation image B of the target material;

[0145] The left vertex C1, the right vertex C2 and the center point O3 of the parallel oblique radiation image C of the target material;

[0146] According to the actual coordinates of points A1 and B1, the distance D1 between A1 and B1 is calculated, and the buried depth of the ore body roof is H1 = D1 / tg(θ).

[0147] According to the actual coordinates of points A2 and B2, the distance D2 between A2 and B2 is calculated, and the buried depth of the ore body bottom plate H2 = D2 / tg(θ).

[0148] According to the actual coordinates of points O1 and O2, the distance D between O1 and O2 and the buried depth of the center of the ore body H=D / tg(θ) are calculated.

[0149] As described above, based on the movement characteristics of the two radiation anomalies, the top plate burial depth H1, the center point burial depth H, and the bottom plate burial depth H2 of the target body (ore body) can be calculated.

[0150] According to the distance D3 between the left vertex C1 and the right vertex C2 of the parallel dip angle radiation image of the target material, the thickness T=D3 of the target body (ore body) can be roughly inferred.

[0151] The parallel dip angle radiation image of the target material is directly emitted from the target material body in the dip angle direction, and the distance between the vertices of the obtained ellipse can be inferred as the thickness of the ore body.

[0152] After the above inversion calculation, the approximate occurrence and morphology of the target substance can be obtained.

[0153] Next, the corresponding mathematical model of the target material is constructed. The mathematical model includes anomaly number, element category, radiation flux density value (radiation intensity value), anomaly distribution area, anomaly position coordinates, anomaly distribution occurrence, anomaly depth range, etc.

[0154] Model establishment First, the extracted radiation anomaly data is numbered and a unique identifier is assigned to each anomaly area. The anomaly number helps to systematically manage each radiation anomaly and facilitate subsequent data processing and analysis. This process provides a clear record for subsequent analysis, allowing specific anomaly data to be clearly referenced during discussions and reports.

[0155] Optionally, in the above features, element category, is to identify the element category of each abnormal area based on the radiation intensity and known geological characteristics. The identification of element category can help geologists understand the composition and properties of the ore body. This is crucial for mineral exploration, because different element distributions can indicate different types of mineral deposits, thus affecting exploration strategies and methods.

[0156] Optionally, in the above features, the radiation flux density value is the radiation flux density value (radiation intensity value) of each abnormal area. The radiation flux density value is a key indicator for evaluating the intensity of radiation anomalies and has a direct impact on subsequent analysis, visualization and decision-making.

[0157] Optionally, in the above features, the anomaly distribution area, the area of ​​each radiation anomaly area. Knowing the anomaly distribution area can help geologists assess the scale of the mineral deposit and make reasonable development plans and resource assessments.

[0158] Optionally, among the above features, the coordinates of the abnormal location, the geographical coordinates of each abnormal area, the recording of the geographical coordinates enables the abnormal area to be accurately located on the map, providing basic data for subsequent exploration and development.

[0159] Optionally, among the above characteristics, the occurrence of abnormal distribution is analyzed to analyze the geological characteristics of each abnormal area, including inclination, strike, etc. The occurrence information of abnormal distribution is very important for understanding the formation and evolution process of ore bodies, which helps to predict the location of other possible ore bodies and guide further exploration work.

[0160] Optionally, among the above features, the anomaly depth range, the depth range of each anomaly area, by understanding the depth distribution of the anomalies, the exploration team can more effectively design drilling plans and select appropriate mining technologies.

[0161] For example, suppose a lepton field radiation exploration is carried out in a mining area. After the mathematical model is established, the following results are obtained:

[0162] Anomaly number: Different radiation anomaly areas are numbered, such as "Anomaly 1", "Anomaly 2", etc.

[0163] Element category identification: It was found that "Anomaly 1" mainly contained uranium, and "Anomaly 2" mainly contained thorium.

[0164] Radiation flux density value record: The radiation intensity of "Abnormal 1" is recorded as 150Bq / m 2 , "Abnormal 2" is 80Bq / m 2 .

[0165] Calculation of abnormal distribution area: The area of ​​"anomaly 1" is 500 square meters, and the area of ​​"anomaly 2" is 300 square meters.

[0166] Anomaly location coordinate record: "Anomaly 1" is located at (longitude X1, latitude Y1), and "Anomaly 2" is located at (longitude X2, latitude Y2).

[0167] Anomaly distribution and occurrence analysis: The analysis shows that "Anomaly 1" is NW-SE trending with a dip of 30 degrees.

[0168] Anomaly Depth Range Estimate: The depth range of "Anomaly 1" is estimated to be 50-100 meters.

[0169] Through the above steps, a visualization model of mining resources was established, and the distribution characteristics of anomalies were automatically analyzed through mathematical models to improve the efficiency and accuracy of geological exploration information visualization.

[0170] It can be understood that the calculation process of obtaining the occurrence and depth of the target body (ore body) through the distribution characteristics of radiation anomalies at different angles is simpler and more accurate. Moreover, due to the uniqueness of subatomic matter, it overcomes the limitations and multi-solutions of geophysical depth inversion calculations and improves the accuracy of the results.

[0171] This example demonstrates how to define the target mining area requirements and select and customize appropriate satellite data in this embodiment; how to construct satellite images and extract subatomic radiation anomalies in the images through subatomic resonance; and how to perform target mineral inversion and mathematical model establishment based on radiation anomalies to achieve visualization of underground target ores.

[0172] From the above description, it can be seen that the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter provided in the embodiment of the present application can perform remote sensing satellite data acquisition operations through the specific scope of the target mining area, set scale, set shooting angle, set time period and set band, and determine the corresponding exploration area remote sensing satellite original film; perform radiation operations on the original film according to a preset subatomic field generator, and perform image enhancement processing on the radiation image of the target material according to a nonlinear algorithm to determine the corresponding target material digital map; determine the corresponding three directions according to the digital map, determine the corresponding three digital images according to the three directions respectively, perform target material inversion calculation and target material model establishment operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization, thereby capturing the subatomic radiation of crustal mineral elements based on satellites, using subatomic characteristics to perform mineral detection and visualization, and improving the efficiency and accuracy of geological exploration.

[0173] In one embodiment of the geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter of the present application, see Figure 2 , and can also include the following:

[0174] Step S201: selecting a scale of the remote sensing satellite image according to the specific range to determine a corresponding set scale, wherein the set scale includes at least one of a large scale, a medium scale, and a small scale;

[0175] Step S202: selecting a shooting angle of the remote sensing satellite image according to the specific range, and determining a corresponding set shooting angle, wherein the selection range of the set shooting angle is 0-180°;

[0176] Step S203: selecting a time period of the remote sensing satellite image according to the specific range, and determining a corresponding set time period, wherein the time interval of the set time period is 30 minutes;

[0177] Step S204: selecting a band of the remote sensing satellite image according to the specific range to determine a corresponding set band, wherein the set band includes at least one of radio frequency, optical, short-wave infrared, long-wave infrared and ultraviolet;

[0178] Step S205: performing remote sensing satellite data acquisition operations according to the set scale, the set shooting angle, the set time period and the set band to determine the corresponding remote sensing satellite digital image of the survey area.

[0179] Optionally, in this embodiment, the specific scope of the target mining area needs to clarify the specific geographical scope and location of the exploration work, including longitude and latitude coordinates and approximate area scope.

[0180] Specifically, remote sensing satellite data acquisition operations should clarify the type, resolution, band, time resolution and other specific requirements of the required satellite data according to the purpose of the survey. Satellites that can provide the required scale, shooting angle, time resolution and band are selected according to the needs. This may involve high-resolution commercial satellites (such as GeoEye and WorldView series), scientific research satellites (such as Landsat and Sentinel series) or satellites for specific missions.

[0181] Specifically, set the scale and customize satellite images of different scales according to the survey needs. This may involve extracting and synthesizing images of different scales from high-resolution satellite data. Use professional software (such as ERDAS IMAGINE, ArcGIS, etc.) to scale, crop and splice images to meet the needs of different scales.

[0182] It is understandable that large-scale satellite images: small range, detailed content, suitable for precise measurement and detailed analysis. In mineral exploration, large-scale satellite images can clearly show the topography, geological structure and other detailed information of the mining area, which is helpful to find direct prospecting signs such as ore outcrops, mineralized alteration zones, etc.

[0183] Medium-scale satellite images: between large-scale and small-scale images, suitable for medium-scale regional surveys. In exploration work, medium-scale satellite images can provide more comprehensive regional geological background information, which helps to understand the structural framework and magmatic rock distribution of the mining area.

[0184] Small-scale satellite images: They show a wide range and a rough outline of the content, and are used to provide an overview of geographic information. Small-scale satellite images can show the geological structure and geomorphic features of the entire exploration area or even a larger area, which helps to grasp the geological background and prospecting direction of the mining area from a macro perspective.

[0185] Specifically, the shooting angle is set to take a satellite image every 3° within the range of 0-180°, ensuring that the satellite can adjust its shooting angle to cover the entire range. Considering the limitations of satellite orbit and attitude control, multiple passes or combining data from multiple satellites may be required to meet this requirement.

[0186] It is understandable that low-angle shooting makes the subject appear taller and more magnificent, increasing the visual impact. In mineral exploration, low-angle satellite images can highlight the height difference of the mining area and enhance the understanding of the topographic features.

[0187] High-angle shooting: Show the overall view and details of the scene, and increase the layering of the picture. Satellite images shot at high angles can fully display the layout and geological structure characteristics of the mining area, which helps to understand the overall geological conditions of the mining area.

[0188] Multi-angle shooting: By shooting at different angles, you can obtain multi-perspective information of the mining area, which helps to more comprehensively understand the geological characteristics and ore body morphology of the mining area. This is of great significance for the three-dimensional modeling of mineral deposits and the analysis of ore body morphology.

[0189] Specifically, set a time period and customize a satellite image every 30 minutes for 24 hours a day. This requires the satellite to have a high-frequency revisit capability or to use multiple satellites for collaborative observation. Ensure that the satellite can take stable images within the specified time period and record the exact time of each shot.

[0190] It is understandable that satellite images of different time periods can have the following observation functions:

[0191] Time series analysis can analyze the dynamic changes of mining areas by acquiring satellite images of different time periods. For example, in mineral exploration, the changes in vegetation coverage and surface water systems in mining areas can be analyzed to infer the geological effects and mineralization processes in mining areas.

[0192] Environmental change monitoring: Satellite images taken at different time periods can also be used to monitor environmental changes in mining areas, such as soil erosion, geological disasters, etc. This is of great significance for assessing environmental risks in mining areas and protecting the ecological environment.

[0193] Specifically, set the bands and customize satellite images in five bands: radio frequency, optical, short-wave infrared, long-wave infrared, and ultraviolet. This requires the satellite to have multi-spectral or hyperspectral imaging capabilities. According to the satellite's band coverage, select the band closest to the requirements for data collection.

[0194] It is understandable that the optical band is mainly used to obtain visible light and infrared band information in the mining area, reflecting the surface coverage and vegetation growth in the mining area. This is of great significance for understanding the natural environment and human activities in the mining area.

[0195] Short-wave infrared band: sensitive to the specific absorption characteristics of minerals, often used for mineral identification and lithology classification. In mineral exploration, short-wave infrared satellite images can reveal the absorption spectrum characteristics of minerals and help discover mineralized alteration zones and ore body outcrops.

[0196] Long-wave infrared band: Mainly used to monitor the surface temperature distribution and heat transfer process. In mineral exploration, long-wave infrared band satellite images can be used to study geothermal anomalies and underground hydrothermal activities in mining areas, providing clues for finding hydrothermal deposits.

[0197] Radio frequency and ultraviolet bands: Although not commonly used in conventional satellite remote sensing in mineral exploration, they have special application value under specific conditions (such as detecting underground pipelines, monitoring atmospheric composition, etc.).

[0198] In summary, satellite images of different scales, shooting angles, time periods, and bands have their own characteristics and functions in remote sensing exploration and monitoring. Together, they provide rich and comprehensive information support for mineral exploration and research in other fields.

[0199] Through step S205, this embodiment successfully customizes satellite data according to exploration needs, taking into account satellite images of different scales, different shooting angles, different time periods, and different bands, providing comprehensive data information support for subsequent accurate target mineral inversion calculation and model construction.

[0200] In one embodiment of the geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter of the present application, see Figure 3 , and can also include the following:

[0201] Step S301: performing Fourier transform operation and image fusion operation on the remote sensing satellite digital image of the survey area to determine the corresponding high-precision remote sensing satellite digital image;

[0202] Step S302: performing laser printing and calibration operations on the high-precision remote sensing satellite digital image to determine the corresponding remote sensing satellite original negative film of the survey area.

[0203] Optionally, a Fourier transform operation is performed to filter the image. The effects of filtering include:

[0204] Noise reduction: Periodic noise will overlap on the source image to form a series of peaks or bright spots, which can be eliminated by bandpass or slot filtering; spike noise can be filtered by Fourier transform.

[0205] Eliminate bad lines and stripes: To eliminate bad lines and stripes in remote sensing images, Fourier transform and low-pass filtering are generally used to eliminate them.

[0206] Optional, image fusion operation aims to fuse multi-source remote sensing data in a unified coordinate system and generate a set of synthetic images using a certain algorithm. This can make up for the lack of information on a single image, expand the application scope of each information, and improve the accuracy of remote sensing image analysis.

[0207] Preferably, the processing of the remote sensing satellite digital image of the survey area may also include:

[0208] Thin cloud processing: Thin clouds appearing in remote sensing images due to weather reasons are weakened.

[0209] Shadow processing: Due to the altitude of the sun, the mountain shadows that appear in remote sensing images can be eliminated using the ratio method.

[0210] Geometric correction: To accurately locate the acquired remote sensing images, they must be geometrically corrected before use. This is done by using the existing accurate geographic coordinate information and projection information to correct the original remote sensing images so that they have accurate geographic coordinate information. In areas with large terrain fluctuations, orthorectification must also be performed. This is done by using existing geographic reference data (topographic maps, control points, etc.) and digital elevation model data (DEM) to correct the original remote sensing images to eliminate or reduce image deformation caused by terrain fluctuations.

[0211] Image enhancement: In order to make the ground object information contained in the remote sensing image more readable, the remote sensing image needs to be enhanced. The histogram transformation is used to count the number of pixels of each brightness in the image. The random distribution of pixel brightness should be normally distributed. The non-normal distribution of the histogram indicates that the image brightness distribution is too bright, too dark, or the brightness is too concentrated, and the image contrast is small. The histogram needs to be adjusted to a normal distribution to improve the image quality.

[0212] Through step S302, this embodiment realizes the special mathematical processing of the remote sensing satellite digital image of the survey area, improves the accuracy and information content of the remote sensing satellite digital image, and lays the foundation for obtaining information from the remote sensing satellite digital image in the future.

[0213] In one embodiment of the geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter of the present application, see Figure 4 , and can also include the following:

[0214] Step S401: performing a radiation operation on the original film according to a subatomic field having the same radiation frequency as the target material emitted by a preset subatomic field generator;

[0215] Step S402: determining a corresponding radiation image of the target material according to the radiation resonance of the target material obtained after the radiation operation is received by a preset photosensitive film.

[0216] Optionally, in this embodiment, this step is performed in a radioactive laboratory. The principle of radiation resonance is that when the leptons in a material body (such as rocks, ores, minerals, etc.) encounter energy fluctuations to form a resonance condition, they will show an energy difference response, thereby radiating a lepton field of a specific frequency. This radiation information can be captured and recorded by remote sensing equipment such as remote sensing satellites. The lepton field can absorb and re-emit radiation energy under the irradiation of a radiation source of a specific wavelength.

[0217] Since the vibration frequencies of the subatomic fields of different substances are different, when extracting the subatomic resonance field, the vibration frequency of the subatomic field generator is selected according to the vibration frequency of the target substance in the vibration frequency spectrum of different substances, and the original film of the remote sensing satellite is radiated to obtain the subatomic distributed radiation resonance field.

[0218] Next, the subatomic distributed radiation resonance field is projected onto the subatomic filter, and the radiation resonance of the target substance is accurately extracted through the filter and the gel of the substance to be collected arranged on the filter.

[0219] Subatomic filters can selectively filter radiation signals of specific wavelengths or energies, thereby extracting lepton radiation characteristics associated with target materials (such as ore bodies). This enables target signals to be more clearly identified against a complex background. In the process of data visualization, subatomic filters can help generate clearer and more informative radiation images, allowing researchers to more intuitively understand the distribution and characteristics of ore bodies.

[0220] The gel of the substance to be collected can effectively concentrate the minerals or compounds in the target sample, which is convenient for subsequent analysis, especially the extraction of trace elements. It focuses on sample processing and the improvement of detection sensitivity, and is used in combination with spectral analysis, chromatographic analysis and other technologies to improve analysis efficiency and accuracy.

[0221] Photographic film responds to radiation energy. By irradiating the target material with radiation resonance, the film can record these radiation signals. The material selection and processing of the film make it sensitive to slight changes in radiation.

[0222] During the experiment, a preset radiation source (such as a laser or other high-energy radiation source) will irradiate the photographic film. The purpose of this process is to enhance the signal and make the radiation characteristics of the target material more obvious. Through appropriate irradiation methods, changes in radiation flux can be effectively recorded.

[0223] When the photographic film receives the radiation signal, the radiation resonance forms corresponding images on the film. These images reflect the radiation characteristics of the target material, including radiation intensity and distribution pattern.

[0224] Optionally, the entire radioactivity test is conducted at three levels:

[0225] The original negative of the satellite image is placed on the top layer, and the satellite image on the top layer is vertically radiated by an external subatomic field generator;

[0226] The subatomic filter is placed in the middle layer to receive the resonance field of the top layer, and the accuracy of the target resonance field is improved through the filter and the gel of the substance to be collected;

[0227] The photosensitive film is placed at the bottom layer, and by arranging a radiation source at the bottom of the photosensitive film, the resonance field can be effectively imaged.

[0228] Preferably, the photosensitive film may be an X-ray film, and the radiation source below the photosensitive film may be an ultraviolet radiation source.

[0229] Through step S402, this embodiment successfully irradiates the original film through the atomic field generator to form a subatomic field resonance of the target substance, and uses the photosensitive film to receive the resonance field to form a radiation image of the target substance on the film.

[0230] In one embodiment of the geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter of the present application, see Figure 5 , and can also include the following:

[0231] Step S501: performing a denoising operation on the target material radiation image according to a nonlinear filtering algorithm to determine a corresponding first material radiation image;

[0232] Step S502: performing an image feature extraction operation on the radiation image of the first material according to a nonlinear image processing algorithm to determine a corresponding enhanced radiation image.

[0233] Optionally, in this embodiment, the nonlinear algorithm is a nonlinear image processing method, which refers to processing an image by using nonlinear mathematical operations and algorithms to improve the quality visualization effect of the image.

[0234] More specifically, nonlinear processing includes the following key steps:

[0235] Image brightness and contrast adjustment: Through nonlinear transformation, the brightness and contrast of the image are optimized to make the image with abnormal radiation intensity distribution more clearly visible.

[0236] Noise Removal: Apply nonlinear filtering technology to remove noise from images and improve the overall image quality.

[0237] Feature description: Use nonlinear image processing technology to perform image edge detection, image segmentation, image enhancement and image compression to better describe the features and structures in the image and improve the visual effect.

[0238] Through step S502, this embodiment successfully enhances the radiation image of the target material through a nonlinear algorithm to obtain an enhanced radiation image, which lays a solid foundation for subsequent digital map drawing and mathematical model establishment.

[0239] In one embodiment of the geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter of the present application, see Figure 6 , and can also include the following:

[0240] Step S601: performing a plane position calibration operation on the enhanced radiation image according to preset geographic coordinates;

[0241] Step S602: performing a vectorization operation on the image after the plane position calibration operation according to a preset vector algorithm to determine a corresponding vectorized radiation image, performing a digitization operation on the vectorized radiation image to determine a corresponding digital map of the target material.

[0242] Optionally, in this embodiment, a GIS geographic information system program is used to perform plane position calibration on the image after nonlinear processing. This process ensures that the extracted radiation intensity image corresponds to the geographic coordinate system and ensures the spatial position of the data is accurate. Through position calibration, the radiation anomaly phenomenon can be correctly located in the actual geographic environment, thereby providing a reliable geographic background for subsequent analysis.

[0243] The nonlinearly processed and calibrated images are vectorized using a geoscientific vectorization program. The vectorization process converts raster images (pixel-based) into vector data (points, lines, and surfaces), making the data more flexible and accurate in display and analysis. Vector data allows for more complex geological analysis and modeling, for example, making it easier to perform spatial analysis and overlay analysis, which improves the usability of the data.

[0244] It is understood that vector data is a representation of geographic information using points, lines, and surfaces. For example, in mineral exploration, the radiation anomaly area of ​​a mining area can be represented by a polygon, and the boundary of this polygon is connected by multiple points (coordinates). Vector data usually has a higher accuracy because it uses coordinates to accurately locate specific geographic features.

[0245] Specifically, relevant data is extracted from the vectorized image, including radiation flux density value, abnormal distribution area, abnormal position coordinates and other information.

[0246] The abnormal radiation range is divided according to the radiation flux density value, and the extracted range-related data is converted into digital format for storage and analysis by the computer system. These data are usually saved in the form of tables or databases. Using the GIS geographic information system, the digitized data is drawn into a digital map to show the spatial distribution of the radiation flux density.

[0247] Through step S602, this embodiment successfully obtains a digital map drawn according to the radiation flux density, which is computable, and the coordinates are calibrated with the geographic location coordinates. The mathematical model calculation and visualization of the target ore body can be performed through the radiation flux density anomaly.

[0248] In one embodiment of the geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter of the present application, see Figure 7 , and can also include the following:

[0249] Step S701: determining a corresponding vertical direction according to the digital map;

[0250] Step S702: determining a corresponding contour anomaly map according to the coordinates in the digital map, performing a profile cutting operation on the contour anomaly map, and determining the inclination and dip angle of the corresponding target material;

[0251] Step S703: determining the corresponding vertical tilt angle direction and parallel tilt angle direction according to the tilt angle.

[0252] Optionally, in this embodiment, the digital map is formed by vertically radiating the original film by the subatomic generator, and the vertical direction is the first direction;

[0253] Connect the numbers with the same radiation energy image in this digital map to form the corresponding target mineral radiation contour anomaly map. In the anomaly map, perform profile cutting on the peak anomaly to restore the dip and inclination of the target mineral. Draw the corresponding tangent to the inclination, and the direction of the tangent is the direction of the inclination. At this time, determine the direction along the inclination as the second direction, and the direction perpendicular to the inclination as the third direction.

[0254] Through step S703, this embodiment successfully obtains three radiation directions, laying a foundation for the subsequent construction of a mathematical model and the inversion of the target ore body.

[0255] In one embodiment of the geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter of the present application, see Figure 8 , and can also include the following:

[0256] Step S801: performing a radiation operation on the original film according to the vertical direction to determine a corresponding vertical radiation image;

[0257] Step S802: performing a radiation operation on the original film according to the vertical inclination direction to determine a corresponding vertical inclination radiation image;

[0258] Step S803: performing a radiation operation on the original film according to the parallel tilt angle direction to determine a corresponding parallel tilt angle radiation image.

[0259] Optionally, in this embodiment, after obtaining the above three directions, the original film is radiated from the above three directions respectively by a subatomic generator to obtain three corresponding radiation images, among which the image radiated from the vertical direction is the vertical radiation image A, that is, the radiation image of the target material obtained in step S102; the image obtained by radiation from the vertical inclination direction is the vertical inclination radiation image B; the image obtained by radiation from the parallel inclination direction is the parallel inclination radiation image C.

[0260] It can be understood that the images radiated from the above three directions appear as three ellipses of different sizes on the plane. At the same time, the above image digitization process is repeated. After the coordinates of the elliptical image are calibrated and vectorized and digitized, the target material can be inverted and calculated through the coordinate points in the ellipse, a mathematical model of the target material can be established, and the target material can be visualized.

[0261] Through step S803, this embodiment successfully radiates from three radiation directions to obtain three radiation maps, and repeats the previous digitization operation to make the three maps computable, laying a computational foundation for subsequent target mineral inversion.

[0262] In one embodiment of the geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter of the present application, see Fig. 9 , and can also include the following:

[0263] Step S901: determining the corresponding target material burial depth according to the vertical inclination radiation image and the vertical radiation image;

[0264] Step S902: determining the corresponding target material thickness according to the parallel tilt angle radiation image;

[0265] Step S903: Determine a corresponding mathematical model of the target material according to the target material burial depth and the target material thickness.

[0266] Optionally, in this embodiment, the target material inversion calculation steps are as follows:

[0267] The left vertex A1, the right vertex A2 and the center point O1 of the vertical radiation image A of the target material;

[0268] The left vertex B1, the right vertex B2 and the center point O2 of the vertical inclination radiation image B of the target material;

[0269] The left vertex C1, the right vertex C2 and the center point O3 of the parallel oblique radiation image C of the target material;

[0270] According to the actual coordinates of points A1 and B1, the distance D1 between A1 and B1 is calculated, and the buried depth of the ore body roof is H1 = D1 / tg(θ).

[0271] According to the actual coordinates of points A2 and B2, the distance D2 between A2 and B2 is calculated, and the buried depth of the ore body bottom plate H2 = D2 / tg(θ).

[0272] According to the actual coordinates of points O1 and O2, the distance D between O1 and O2 and the buried depth of the center of the ore body H=D / tg(θ) are calculated.

[0273] As described above, based on the movement characteristics of the two radiation anomalies, the top plate burial depth H1, the center point burial depth H, and the bottom plate burial depth H2 of the target body (ore body) can be calculated.

[0274] According to the distance D3 between the left vertex C1 and the right vertex C2 of the parallel dip angle radiation image of the target material, the thickness T=D3 of the target body (ore body) can be roughly inferred.

[0275] The parallel dip angle radiation image of the target material is directly emitted from the target material body in the dip angle direction, and the distance between the vertices of the obtained ellipse can be inferred as the thickness of the ore body.

[0276] After the above inversion calculation, the approximate occurrence and morphology of the target substance can be obtained.

[0277] Next, the corresponding mathematical model of the target material is constructed. The mathematical model includes anomaly number, element category, radiation flux density value (radiation intensity value), anomaly distribution area, anomaly position coordinates, anomaly distribution occurrence, anomaly depth range, etc.

[0278] Model establishment First, the extracted radiation anomaly data is numbered and a unique identifier is assigned to each anomaly area. The anomaly number helps to systematically manage each radiation anomaly and facilitate subsequent data processing and analysis. This process provides a clear record for subsequent analysis, allowing specific anomaly data to be clearly referenced during discussions and reports.

[0279] Optionally, in the above features, element category, is to identify the element category of each abnormal area based on the radiation intensity and known geological characteristics. The identification of element category can help geologists understand the composition and properties of the ore body. This is crucial for mineral exploration, because different element distributions can indicate different types of mineral deposits, thus affecting exploration strategies and methods.

[0280] Optionally, in the above features, the radiation flux density value is the radiation flux density value (radiation intensity value) of each abnormal area. The radiation flux density value is a key indicator for evaluating the intensity of radiation anomalies and has a direct impact on subsequent analysis, visualization and decision-making.

[0281] Optionally, in the above features, the anomaly distribution area, the area of ​​each radiation anomaly area. Knowing the anomaly distribution area can help geologists assess the scale of the mineral deposit and make reasonable development plans and resource assessments.

[0282] Optionally, among the above features, the coordinates of the abnormal location, the geographical coordinates of each abnormal area, the recording of the geographical coordinates enables the abnormal area to be accurately located on the map, providing basic data for subsequent exploration and development.

[0283] Optionally, among the above characteristics, the occurrence of abnormal distribution is analyzed to analyze the geological characteristics of each abnormal area, including inclination, strike, etc. The occurrence information of abnormal distribution is very important for understanding the formation and evolution process of ore bodies, which helps to predict the location of other possible ore bodies and guide further exploration work.

[0284] Optionally, among the above features, the anomaly depth range, the depth range of each anomaly area, by understanding the depth distribution of the anomalies, the exploration team can more effectively design drilling plans and select appropriate mining technologies.

[0285] For example, suppose a lepton field radiation exploration is carried out in a mining area. After the mathematical model is established, the following results are obtained:

[0286] Anomaly number: Different radiation anomaly areas are numbered, such as "Anomaly 1", "Anomaly 2", etc.

[0287] Element category identification: It was found that "Anomaly 1" mainly contained uranium, and "Anomaly 2" mainly contained thorium.

[0288] Radiation flux density value record: The radiation intensity of "Abnormal 1" is recorded as 150Bq / m 2 , "Abnormal 2" is 80Bq / m 2 .

[0289] Calculation of abnormal distribution area: The area of ​​"anomaly 1" is 500 square meters, and the area of ​​"anomaly 2" is 300 square meters.

[0290] Anomaly location coordinate record: "Anomaly 1" is located at (longitude X1, latitude Y1), and "Anomaly 2" is located at (longitude X2, latitude Y2).

[0291] Anomaly distribution and occurrence analysis: The analysis shows that "Anomaly 1" is NW-SE trending with a dip of 30 degrees.

[0292] Anomaly Depth Range Estimate: The depth range of "Anomaly 1" is estimated to be 50-100 meters.

[0293] Through step S903, this embodiment successfully establishes a visualization model of mining resources, automatically analyzes the distribution characteristics of anomalies through mathematical models, and improves the efficiency and accuracy of geological exploration information visualization.

[0294] In order to capture the subatomic radiation of crustal mineral elements based on satellites, use subatomic properties to detect and visualize minerals, and improve the efficiency and accuracy of geological exploration, the present application provides an embodiment of a geological exploration device based on the intrinsic subatomic wave radiation characteristics of matter for realizing all or part of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter, see Fig.10The geological exploration device based on the intrinsic subatomic wave radiation characteristics of matter specifically includes the following contents:

[0295] The original negative film customization module 10 is used to determine the specific scope of the target mining area, perform remote sensing satellite data acquisition operations according to the specific scope, set scale, set shooting angle, set time period and set band, determine the corresponding remote sensing satellite digital image of the exploration area, perform special mathematical calculation processing on the remote sensing satellite digital image of the exploration area, and perform laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing to determine the corresponding remote sensing satellite original negative film of the exploration area;

[0296] The radiation image extraction module 20 is used to perform a radiation operation on the original film according to a preset subatomic field generator to determine a corresponding target material radiation image, perform image enhancement processing on the target material radiation image according to a nonlinear algorithm to determine a corresponding enhanced radiation image, and perform a digitization operation on the enhanced radiation image according to preset geographic coordinates and a preset vector algorithm to determine a corresponding target material digital map;

[0297] The mineral mathematical model building module 30 is used to determine the corresponding three directions according to the digital map, perform radiation operations on the original film according to the three directions respectively, determine the corresponding three digital images, perform target material inversion calculation and target material model building operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization.

[0298] From the above description, it can be seen that the geological exploration device based on the intrinsic subatomic wave radiation characteristics of matter provided in the embodiment of the present application can perform remote sensing satellite data acquisition operations through the specific scope of the target mining area, set scale, set shooting angle, set time period and set band, and determine the original remote sensing satellite film of the corresponding exploration area; perform radiation operations on the original film according to the preset subatomic field generator, and perform image enhancement processing on the radiation image of the target material according to the nonlinear algorithm to determine the corresponding digital map of the target material; determine the corresponding three directions according to the digital map, determine the corresponding three digital images according to the three directions respectively, perform target material inversion calculation and target material model establishment operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization, thereby capturing the subatomic radiation of crustal mineral elements based on satellites, using subatomic characteristics to detect and visualize minerals, and improve the efficiency and accuracy of geological exploration.

[0299] From the hardware level, in order to capture the subatomic radiation of crustal mineral elements based on satellites, use subatomic properties to detect and visualize minerals, and improve the efficiency and accuracy of geological exploration, the present application provides an embodiment of an electronic device for implementing all or part of the contents of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter, and the electronic device specifically includes the following contents:

[0300] Processor, memory, communication interface and bus; wherein the processor, memory and communication interface communicate with each other through the bus; the communication interface is used to realize information transmission between the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter and related equipment such as the core business system, user terminal and related database; the logic controller can be a desktop computer, a tablet computer and a mobile terminal, etc., and the present embodiment is not limited thereto. In the present embodiment, the logic controller can be implemented with reference to the embodiment of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the embodiment, and the embodiment of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter, and the content thereof is incorporated herein, and the repeated parts are not repeated.

[0301] It is understandable that the user terminal may include a smart phone, a tablet electronic device, a network set-top box, a portable computer, a desktop computer, a personal digital assistant (PDA), a vehicle-mounted device, a smart wearable device, etc. Among them, the smart wearable device may include smart glasses, a smart watch, a smart bracelet, etc.

[0302] In practical applications, part of the geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter can be executed on the electronic device side as described above, or all operations can be completed in the client device. The specific selection can be based on the processing capability of the client device and the limitations of the user's usage scenario. This application does not limit this. If all operations are completed in the client device, the client device may also include a processor.

[0303] The client device may have a communication module (i.e., a communication unit) that can communicate with a remote server to achieve data transmission with the server. The server may include a server on the task scheduling center side, and other implementation scenarios may also include a server on an intermediate platform, such as a server on a third-party server platform that has a communication link with the task scheduling center server. The server may include a single computer device, or a server cluster consisting of multiple servers, or a server structure of a distributed device.

[0304] Fig.11FIG. 9 is a schematic block diagram of the system structure of the electronic device 9600 according to an embodiment of the present application. Fig.11 As shown, the electronic device 9600 may include a central processor 9100 and a memory 9140; the memory 9140 is coupled to the central processor 9100. It is worth noting that Fig.11 is exemplary; other types of structures may also be used to supplement or replace this structure to implement telecommunication functions or other functions.

[0305] In one embodiment, the geological exploration method function based on the intrinsic subatomic wave radiation characteristics of matter can be integrated into the central processor 9100. The central processor 9100 can be configured to perform the following control:

[0306] Step S101: determining the specific scope of the target mining area, performing remote sensing satellite data acquisition operations according to the specific scope, setting the scale, setting the shooting angle, setting the time period and setting the band, determining the corresponding remote sensing satellite digital image of the exploration area, performing special mathematical calculation processing on the remote sensing satellite digital image of the exploration area, and performing laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing, and determining the corresponding remote sensing satellite original negative of the exploration area;

[0307] Step S102: performing radiation operation on the original film according to a preset subatomic field generator to determine a corresponding target material radiation image, performing image enhancement processing on the target material radiation image according to a nonlinear algorithm to determine a corresponding enhanced radiation image, performing digitization operation on the enhanced radiation image according to preset geographic coordinates and a preset vector algorithm to determine a corresponding target material digital map;

[0308] Step S103: Determine three corresponding directions according to the digital map, perform radiation operations on the original film according to the three directions respectively, determine three corresponding digital images, perform target material inversion calculation and target material model establishment operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization.

[0309] From the above description, it can be seen that the electronic device provided in the embodiment of the present application performs remote sensing satellite data acquisition operations through the specific scope of the target mining area, sets the scale, sets the shooting angle, sets the time period and sets the band, and determines the original remote sensing satellite film of the corresponding exploration area; performs radiation operations on the original film according to the preset subatomic field generator, and performs image enhancement processing on the radiation image of the target material according to the nonlinear algorithm to determine the corresponding digital map of the target material; determines the corresponding three directions according to the digital map, determines the corresponding three digital images according to the three directions respectively, performs target material inversion calculation and target material model establishment operations according to the three digital images, determines the corresponding mathematical model of the target material, and realizes visualization of the target material, thereby capturing the subatomic radiation of crustal mineral elements based on satellites, and using subatomic characteristics to detect and visualize minerals, thereby improving the efficiency and accuracy of geological exploration.

[0310] In another embodiment, the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter can be configured separately from the central processor 9100. For example, the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter can be configured as a chip connected to the central processor 9100, and the function of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter can be realized through the control of the central processor.

[0311] like Fig.11 As shown, the electronic device 9600 may also include: a communication module 9110, an input unit 9120, an audio processor 9130, a display 9160, and a power supply 9170. It is worth noting that the electronic device 9600 does not necessarily have to include Fig.11 In addition, the electronic device 9600 may also include Fig.11 For components not shown, reference may be made to the prior art.

[0312] like Fig.11 As shown, the central processing unit 9100 is sometimes also referred to as a controller or an operation control, and may include a microprocessor or other processor device and / or logic device. The central processing unit 9100 receives input and controls the operation of various components of the electronic device 9600.

[0313] The memory 9140 may be, for example, one or more of a cache, a flash memory, a hard drive, a removable medium, a volatile memory, a non-volatile memory or other suitable devices. The above-mentioned information related to the failure may be stored, and a program for executing the relevant information may also be stored. The CPU 9100 may execute the program stored in the memory 9140 to implement information storage or processing, etc.

[0314] The input unit 9120 provides input to the central processing unit 9100. The input unit 9120 is, for example, a key or a touch input device. The power supply 9170 is used to provide power to the electronic device 9600. The display 9160 is used to display display objects such as images and texts. The display may be, for example, an LCD display, but is not limited thereto.

[0315] The memory 9140 may be a solid-state memory, such as a read-only memory (ROM), a random access memory (RAM), a SIM card, etc. It may also be a memory that saves information even when the power is off, can be selectively erased, and is provided with more data, examples of which are sometimes referred to as EPROMs, etc. The memory 9140 may also be some other type of device. The memory 9140 includes a buffer memory 9141 (sometimes referred to as a buffer). The memory 9140 may include an application / function storage unit 9142, which is used to store application programs and function programs or processes for executing the operation of the electronic device 9600 through the central processor 9100.

[0316] The memory 9140 may also include a data storage unit 9143 for storing data, such as contacts, digital data, pictures, sounds, and / or any other data used by the electronic device. The driver storage unit 9144 of the memory 9140 may include various drivers for communication functions of the electronic device and / or for executing other functions of the electronic device (such as messaging applications, address book applications, etc.).

[0317] The communication module 9110 is a transmitter / receiver that sends and receives signals via the antenna 9111. The communication module 9110 is coupled to the central processor 9100 to provide input signals and receive output signals, which may be the same as the case of a conventional mobile communication terminal.

[0318] Based on different communication technologies, multiple communication modules 9110 may be provided in the same electronic device, such as a cellular network module, a Bluetooth module and / or a wireless local area network module, etc. The communication module 9110 is also coupled to a speaker 9131 and a microphone 9132 via an audio processor 9130 to provide an audio output via the speaker 9131 and receive an audio input from the microphone 9132, thereby realizing a common telecommunication function. The audio processor 9130 may include any suitable buffer, decoder, amplifier, etc. In addition, the audio processor 9130 is also coupled to the central processor 9100, so that recording can be performed on the machine through the microphone 9132, and the sound stored on the machine can be played through the speaker 9131.

[0319] The embodiments of the present application also provide a computer-readable storage medium capable of implementing all the steps of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the above-mentioned embodiments, where the execution subject is a server or a client. The computer-readable storage medium stores a computer program, and when the computer program is executed by a processor, all the steps of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the above-mentioned embodiments are implemented. For example, when the processor executes the computer program, the following steps are implemented:

[0320] Step S101: determining the specific scope of the target mining area, performing remote sensing satellite data acquisition operations according to the specific scope, setting the scale, setting the shooting angle, setting the time period and setting the band, determining the corresponding remote sensing satellite digital image of the exploration area, performing special mathematical calculation processing on the remote sensing satellite digital image of the exploration area, and performing laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing, and determining the corresponding remote sensing satellite original negative of the exploration area;

[0321] Step S102: performing radiation operation on the original film according to a preset subatomic field generator to determine a corresponding target material radiation image, performing image enhancement processing on the target material radiation image according to a nonlinear algorithm to determine a corresponding enhanced radiation image, performing digitization operation on the enhanced radiation image according to preset geographic coordinates and a preset vector algorithm to determine a corresponding target material digital map;

[0322] Step S103: Determine three corresponding directions according to the digital map, perform radiation operations on the original film according to the three directions respectively, determine three corresponding digital images, perform target material inversion calculation and target material model establishment operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization.

[0323] From the above description, it can be seen that the computer-readable storage medium provided in the embodiment of the present application performs remote sensing satellite data acquisition operations through the specific scope of the target mining area, sets the scale, sets the shooting angle, sets the time period, and sets the band to determine the original remote sensing satellite film of the corresponding exploration area; performs radiation operations on the original film according to the preset subatomic field generator, and performs image enhancement processing on the radiation image of the target material according to the nonlinear algorithm to determine the corresponding digital map of the target material; determines the corresponding three directions according to the digital map, determines the corresponding three digital images according to the three directions respectively, performs target material inversion calculation and target material model establishment operations according to the three digital images, determines the corresponding mathematical model of the target material, and realizes visualization of the target material, thereby enabling the satellite to capture the subatomic radiation of crustal mineral elements, and utilizes the subatomic characteristics to perform mineral detection and visualization, thereby improving the efficiency and accuracy of geological exploration.

[0324] The embodiments of the present application also provide a computer program product capable of implementing all the steps of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter in the above embodiments, where the execution subject is a server or a client. When the computer program / instruction is executed by a processor, the steps of the geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter are implemented. For example, the computer program / instruction implements the following steps:

[0325] Step S101: determining the specific scope of the target mining area, performing remote sensing satellite data acquisition operations according to the specific scope, setting the scale, setting the shooting angle, setting the time period and setting the band, determining the corresponding remote sensing satellite digital image of the exploration area, performing special mathematical calculation processing on the remote sensing satellite digital image of the exploration area, and performing laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing, and determining the corresponding remote sensing satellite original negative of the exploration area;

[0326] Step S102: performing radiation operation on the original film according to a preset subatomic field generator to determine a corresponding target material radiation image, performing image enhancement processing on the target material radiation image according to a nonlinear algorithm to determine a corresponding enhanced radiation image, performing digitization operation on the enhanced radiation image according to preset geographic coordinates and a preset vector algorithm to determine a corresponding target material digital map;

[0327] Step S103: Determine three corresponding directions according to the digital map, perform radiation operations on the original film according to the three directions respectively, determine three corresponding digital images, perform target material inversion calculation and target material model establishment operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization.

[0328] From the above description, it can be seen that the computer program product provided in the embodiment of the present application performs remote sensing satellite data acquisition operations through the specific scope of the target mining area, sets the scale, sets the shooting angle, sets the time period, and sets the band to determine the original remote sensing satellite film of the corresponding exploration area; performs radiation operations on the original film according to the preset subatomic field generator, and performs image enhancement processing on the radiation image of the target material according to the nonlinear algorithm to determine the corresponding digital map of the target material; determines the corresponding three directions according to the digital map, determines the corresponding three digital images according to the three directions respectively, performs target material inversion calculation and target material model establishment operations according to the three digital images, determines the corresponding mathematical model of the target material, and realizes visualization of the target material, thereby capturing the subatomic radiation of crustal mineral elements based on satellites, and using subatomic characteristics to detect and visualize minerals, thereby improving the efficiency and accuracy of geological exploration.

[0329] It will be appreciated by those skilled in the art that embodiments of the present invention may be provided as methods, devices, or computer program products. Therefore, the present invention may take the form of a complete hardware embodiment, a complete software embodiment, or an embodiment combining software and hardware. Moreover, the present invention may take the form of a computer program product implemented on one or more computer-usable storage media (including but not limited to disk storage, CD-ROM, optical storage, etc.) containing computer-usable program code.

[0330] The present invention is described with reference to flowcharts and / or block diagrams of methods, devices (apparatus), and computer program products according to embodiments of the present invention. It should be understood that each process and / or block in the flowchart and / or block diagram, as well as the combination of processes and / or blocks in the flowchart and / or block diagram, can be implemented by computer program instructions. These computer program instructions can be provided to a processor of a general-purpose computer, a special-purpose computer, an embedded processor, or other programmable data processing device to generate a machine, so that the instructions executed by the processor of the computer or other programmable data processing device generate instructions for implementing the processes in the flowchart and / or block diagram. Figure 1 A process or multiple processes and / or boxes Figure 1 A device that provides the functions specified in a block or multiple blocks.

[0331] These computer program instructions may also be stored in a computer-readable memory capable of directing a computer or other programmable data processing device to operate in a specific manner, so that the instructions stored in the computer-readable memory produce an article of manufacture comprising an instruction device, which implements the process Figure 1 A process or multiple processes and / or boxes Figure 1 A function specified in one or more boxes.

[0332] These computer program instructions can also be loaded onto a computer or other programmable data processing device so that a series of operating steps are executed on the computer or other programmable device to produce a computer-implemented process, thereby providing instructions for implementing the process. Figure 1 A process or multiple processes and / or boxes Figure 1 The steps for the functions specified in one or more boxes.

[0333] The present invention uses specific embodiments to illustrate the principles and implementation methods of the present invention. The description of the above embodiments is only used to help understand the method of the present invention and its core idea. At the same time, for those skilled in the art, according to the idea of ​​the present invention, there will be changes in the specific implementation methods and application scope. In summary, the content of this specification should not be understood as a limitation on the present invention.

Claims

1. A geological exploration method based on the intrinsic subatomic wave radiation characteristics of matter, characterized in that: The method comprises: Determine the specific scope of the target mining area, perform remote sensing satellite data acquisition operations according to the specific scope, set scale, set shooting angle, set time period and set band, determine the corresponding remote sensing satellite digital image of the exploration area, perform special mathematical calculation processing on the remote sensing satellite digital image of the exploration area, and perform laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing to determine the corresponding remote sensing satellite original negative of the exploration area; Performing radiation operation on the original film according to a preset subatomic field generator to determine a corresponding radiation image of the target substance, performing image enhancement processing on the radiation image of the target substance according to a nonlinear algorithm to determine a corresponding enhanced radiation image, and performing digitization operation on the enhanced radiation image according to preset geographic coordinates and a preset vector algorithm to determine a corresponding digital map of the target substance; Determine the corresponding three directions according to the digital map, perform radiation operations on the original film according to the three directions respectively, determine the corresponding three digital images, perform target material inversion calculation and target material model establishment operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization.

2. The geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter according to claim 1 is characterized in that: The remote sensing satellite data acquisition operation is performed according to the specific range, the set scale, the set shooting angle, the set time period and the set band to determine the corresponding remote sensing satellite digital image of the survey area, including: Selecting a scale of the remote sensing satellite image according to the specific range to determine a corresponding set scale, wherein the set scale includes at least one of a large scale, a medium scale, and a small scale; Selecting a shooting angle of the remote sensing satellite image according to the specific range to determine a corresponding set shooting angle, wherein the selection range of the set shooting angle is 0-180°; Selecting a time period of the remote sensing satellite image according to the specific range to determine a corresponding set time period, wherein the time interval of the set time period is 30 minutes; Selecting a band of the remote sensing satellite image according to the specific range to determine a corresponding set band, wherein the set band includes at least one of radio frequency, optical, short-wave infrared, long-wave infrared and ultraviolet; The remote sensing satellite data acquisition operation is performed according to the set scale, set shooting angle, set time period and set band to determine the corresponding remote sensing satellite digital image of the survey area.

3. The geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter according to claim 1, characterized in that: The step of performing special mathematical calculation processing on the remote sensing satellite digital image of the survey area, and performing laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing to determine the corresponding remote sensing satellite original negative film of the survey area includes: Performing Fourier transform operation and image fusion operation on the remote sensing satellite digital image of the survey area to determine the corresponding high-precision remote sensing satellite digital image; Laser printing and calibration operations are performed on the high-precision remote sensing satellite digital image to determine the corresponding remote sensing satellite original negative film of the survey area.

4. The geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter according to claim 1, characterized in that: The step of performing a radiation operation on the original film according to a preset subatomic field generator to determine a corresponding radiation image of the target substance includes: Performing a radiation operation on the original film according to a subatomic field emitted by a preset subatomic field generator having the same radiation frequency as that of the target material; According to the radiation resonance of the target substance obtained after the radiation operation is received by the preset photosensitive film, a corresponding radiation image of the target substance is determined.

5. The geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter according to claim 1, characterized in that: The performing image enhancement processing on the radiation image of the target material according to the nonlinear algorithm to determine the corresponding enhanced radiation image includes: Performing a denoising operation on the target material radiation image according to a nonlinear filtering algorithm to determine a corresponding first material radiation image; An image feature extraction operation is performed on the radiation image of the first material according to a nonlinear image processing algorithm to determine a corresponding enhanced radiation image.

6. The geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter according to claim 1, characterized in that: The enhanced radiation image is digitized according to the preset geographic coordinates and the preset vector algorithm to determine the corresponding digital map of the target material; Performing a plane position calibration operation on the enhanced radiation image according to preset geographic coordinates; A vectorization operation is performed on the image after the plane position calibration operation according to a preset vector algorithm to determine a corresponding vectorized radiation image, and a digitization operation is performed on the vectorized radiation image to determine a corresponding digital map of the target material.

7. The geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter according to claim 1, characterized in that: The determining of the corresponding three directions according to the digital map includes: Determining a corresponding vertical direction according to the digital map; Determine a corresponding contour anomaly map according to the coordinates in the digital map, perform a profile cutting operation on the contour anomaly map, and determine the inclination and dip angle of the corresponding target material; The corresponding vertical tilt angle direction and parallel tilt angle direction are determined according to the tilt angle.

8. The geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter according to claim 1, characterized in that: The step of performing radiation operations on the original film according to the three directions to determine the corresponding three digital images includes: Performing a radiation operation on the original film according to the vertical direction to determine a corresponding vertical radiation image; Performing a radiation operation on the original film according to the vertical inclination direction to determine a corresponding vertical inclination radiation image; The original film is subjected to a radiation operation according to the parallel tilt angle direction to determine a corresponding parallel tilt angle radiation image.

9. The geological prospecting method based on the intrinsic subatomic wave radiation characteristics of matter according to claim 1, characterized in that: The target material inversion calculation and target material model establishment operations are performed according to the three digital images to determine the corresponding target material mathematical model, including: Determine the corresponding target material burial depth according to the vertical inclination radiation image and the vertical radiation image; Determine the corresponding target material thickness according to the parallel tilt angle radiation image; A corresponding mathematical model of the target material is determined according to the buried depth of the target material and the thickness of the target material.

10. A geological exploration device based on the intrinsic subatomic wave radiation characteristics of matter, characterized in that: The device comprises: The original negative film customization module is used to determine the specific scope of the target mining area, perform remote sensing satellite data acquisition operations according to the specific scope, set scale, set shooting angle, set time period and set band, determine the corresponding remote sensing satellite digital image of the exploration area, perform special mathematical calculation processing on the remote sensing satellite digital image of the exploration area, and perform laser printing and calibration operations on the digital image obtained after the special mathematical calculation processing to determine the corresponding remote sensing satellite original negative film of the exploration area; A radiation image extraction module is used to perform a radiation operation on the original film according to a preset subatomic field generator to determine a corresponding target material radiation image, perform image enhancement processing on the target material radiation image according to a nonlinear algorithm to determine a corresponding enhanced radiation image, and perform a digitization operation on the enhanced radiation image according to preset geographic coordinates and a preset vector algorithm to determine a corresponding target material digital map; The mineral mathematical model building module is used to determine the corresponding three directions according to the digital map, perform radiation operations on the original film according to the three directions respectively, determine the corresponding three digital images, perform target material inversion calculation and target material model building operations according to the three digital images, determine the corresponding target material mathematical model, and realize target material visualization.

Images