Methods and apparatus for inverting underground exploration targets

Abstract

This application provides a method and apparatus for inverting underground exploration targets. The method includes: acquiring original negatives of underground exploration remote sensing satellite images; performing vertical radiometric operations on the original negatives using a preset subatomic field generator to determine the corresponding vertical radiometric image of the target material and the dip and tilt angle of the target material; performing radiometric operations on the original negatives using the subatomic field generator and the tilt angle to determine the corresponding vertical tilt radiometric image and parallel tilt radiometric image of the target material; determining the corresponding burial depth of the target material based on the vertical tilt radiometric image and the vertical radiometric image of the target material; determining the corresponding thickness of the target material based on the parallel tilt radiometric image of the target material; and determining the corresponding target material inversion result based on the burial depth and the thickness of the target material. This application can improve the accuracy and efficiency of underground exploration inversion results based on the characteristics of subatomic radiation.

Description

Technical Field

[0001] This application relates to the field of data processing, specifically to a method and apparatus for inverting underground exploration targets. Background Technology

[0002] The main method for depth exploration in geological exploration is geophysical exploration, which is the process of inferring underground structures by inverting depth calculations from geophysical data.

[0003] The depth calculation in geophysical inversion currently mainly involves the joint inversion of various geophysical data, which is an important quantitative interpretation method for integrated geophysical research. Each geophysical method has limitations, and the interpretation of a specific exploration target is often multifaceted. By utilizing different physical properties to describe the same target from various perspectives, the interpretation results can be made closer to the actual geological conditions. Therefore, the research and development direction of geophysical joint inversion mainly focuses on how to utilize the joint inversion of various geophysical data to improve the accuracy and reliability of the interpretation results.

[0004] However, the main shortcomings of geophysical inversion lie in overcoming the limitations and multiple solutions of various geophysical methods to improve the accuracy and efficiency of inversion. Although new technologies such as deep learning have provided new ideas and methods for geophysical inversion, such as using deep learning technology to process large amounts of heterogeneous multimodal data in geophysical exploration, the application of these technologies is still in the exploratory and developmental stage, and the challenge lies in how to effectively integrate these new technologies into the existing geophysical inversion workflow.

[0005] In summary, the shortcomings of geophysical inversion mainly lie in the limitations and ambiguity of geophysical methods, how to improve the accuracy of interpretation results, and the challenges of integrating and applying new technologies. There is an urgent need for a subsurface exploration target inversion method that can overcome the limitations and ambiguity of geophysical depth inversion calculations, thereby improving the accuracy and efficiency of subsurface exploration results. Summary of the Invention

[0006] To address the problems in the prior art, this application provides a method and apparatus for inverting underground exploration targets, which can improve the accuracy and efficiency of underground exploration inversion results based on subatomic radiation characteristics.

[0007] To solve at least one of the above problems, this application provides the following technical solution:

[0008] Firstly, this application provides a method for inverting underground exploration targets, including:

[0009] The original negative of remote sensing satellite image of underground exploration target is acquired. The original negative is subjected to vertical radiometric operation according to a preset subatomic field generator to determine the vertical radiometric image of the target material. The dip and tilt angle of the target material are determined according to the vertical radiometric image of the target material.

[0010] The original film is irradiated using the subatomic field generator and the tilt angle to determine the corresponding vertical tilt angle irradiation image and the target material parallel tilt angle irradiation image. The target material burial depth is determined based on the target material vertical tilt angle irradiation image and the target material vertical irradiation image. The target material thickness is determined based on the target material parallel tilt angle irradiation image.

[0011] Based on the burial depth and thickness of the target material, a target material inversion operation is performed to determine the corresponding target material inversion result.

[0012] Further, determining the tendency and tilt angle of the target material based on the vertical radiation image of the target material includes:

[0013] The vertical radiation image of the target material is digitally processed to determine the corresponding vertical radiation contour anomaly map.

[0014] The vertical radiation contour anomaly map is subjected to a profile cutting operation, and the tendency and dip angle of the corresponding target material are determined based on the profile map obtained after the profile cutting operation.

[0015] Further, the step of performing a radiation operation on the original film based on the subatomic field generator and the tilt angle to determine the corresponding target material vertical tilt angle radiation image and target material parallel tilt angle radiation image includes:

[0016] The corresponding vertical tilt direction and parallel tilt direction are determined based on the tilt angle.

[0017] The subatomic field generator performs radiation operations on the original film from the vertical tilt direction and the parallel tilt direction respectively to determine the corresponding vertical tilt radiation image and parallel tilt radiation image of the target material.

[0018] Further, determining the corresponding burial depth of the target material based on the vertical tilt radiation image of the target material and the vertical radiation image of the target material includes:

[0019] The burial depth of the top plate of the target material is determined based on the distance between the left vertices of the vertical tilt radiation image of the target material and the angle of the tilt.

[0020] The burial depth of the target material's center point is determined based on the distance between the center points of the vertical tilt radiation images of the target material and the angle of the tilt.

[0021] The corresponding burial depth of the target material's base plate is determined based on the distance between the right vertices of the vertical tilt radiation image of the target material and the angle of the tilt.

[0022] The corresponding target material burial depth is determined based on the burial depth of the top plate of the target material, the burial depth of the center point of the target material, and the burial depth of the bottom plate of the target material.

[0023] Further, determining the corresponding target material thickness based on the parallel tilt angle radiation image of the target material includes:

[0024] The left and right vertices of the target material's parallel tilt angle radiation image are determined based on the target material's parallel tilt angle radiation image.

[0025] The thickness of the target material is determined based on the straight-line distance between the left and right vertices.

[0026] Further, the step of digitally processing the vertical radiation image of the target material to determine the corresponding vertical radiation contour anomaly map includes:

[0027] The vertical radiation image of the target material is enhanced using a nonlinear image processing algorithm to determine the corresponding enhanced radiation image.

[0028] The enhanced image is digitally processed based on preset geographic coordinates and a preset vector algorithm to determine the corresponding vertical radiation contour anomaly map.

[0029] Further, the step of performing vertical radiation operation on the original film according to a preset subatomic field generator to determine the corresponding target material vertical radiation image includes:

[0030] The original film is subjected to vertical radiation operation based on a subatomic field emitted by a preset subatomic field generator that has the same radiation frequency as the target material.

[0031] The subatomic field radiation resonance obtained after the vertical radiation operation is received by a preset subatomic filter, and the subatomic field radiation resonance is filtered to determine the corresponding target material vertical radiation resonance.

[0032] Based on the vertical radiation resonance of the target material received by the preset photosensitive film, the corresponding vertical radiation image of the target material is determined.

[0033] Secondly, this application provides an underground exploration target inversion device, comprising:

[0034] The target material occurrence determination module is used to acquire the original negative of remote sensing satellite images of underground exploration targets, perform vertical radiation operation on the original negative according to a preset subatomic field generator, determine the corresponding target material vertical radiation image, and determine the dip and dip angle of the target material according to the target material vertical radiation image.

[0035] The target material morphology determination module is used to perform radiation operation on the original film according to the subatomic field generator and the tilt angle, determine the corresponding target material vertical tilt angle radiation image and target material parallel tilt angle radiation image, determine the corresponding target material burial depth according to the target material vertical tilt angle radiation image and target material vertical radiation image, and determine the corresponding target material thickness according to the target material parallel tilt angle radiation image;

[0036] The target material inversion module is used to perform target material inversion operations based on the burial depth and thickness of the target material, and determine the corresponding target material inversion results.

[0037] Thirdly, this application provides an electronic device, including a memory, a processor, and a computer program stored in the memory and executable on the processor, wherein the processor executes the program to implement the steps of the underground exploration target inversion method.

[0038] Fourthly, this application provides a computer-readable storage medium having a computer program stored thereon, which, when executed by a processor, implements the steps of the underground exploration target inversion method.

[0039] Fifthly, this application provides a computer program product, including a computer program / instructions, which, when executed by a processor, implement the steps of the underground exploration target inversion method.

[0040] As can be seen from the above technical solution, this application provides a method and apparatus for inverting underground exploration targets. By acquiring the original film of underground exploration remote sensing satellite images, a vertical radiometric operation is performed on the original film using a preset subatomic field generator to determine the corresponding vertical radiometric image of the target material and the dip and tilt angle of the target material. The original film is then radiometrically operated using the subatomic field generator and the tilt angle to determine the corresponding vertical tilt radiometric image and parallel tilt radiometric image of the target material. The burial depth of the target material is determined based on the vertical tilt radiometric image and the vertical radiometric image of the target material, and the thickness of the target material is determined based on the parallel tilt radiometric image. Finally, the inversion result of the target material is determined based on the burial depth and the thickness of the target material. This improves the accuracy and efficiency of underground exploration inversion results based on the characteristics of subatomic radiation. Attached Figure Description

[0041] To more clearly illustrate the technical solutions in the embodiments of this application or the prior art, the drawings used in the description of the embodiments or the prior art will be briefly introduced below. Obviously, the drawings described below are some embodiments of this application. For those skilled in the art, other drawings can be obtained based on these drawings without creative effort.

[0042] Figure 1 This is one of the flowcharts illustrating the underground exploration target inversion method in this application embodiment;

[0043] Figure 2 This is the second flowchart illustrating the underground exploration target inversion method in this application embodiment;

[0044] Figure 3 This is the third flowchart illustrating the underground exploration target inversion method in this application embodiment;

[0045] Figure 4 This is the fourth flowchart illustrating the underground exploration target inversion method in this application embodiment;

[0046] Figure 5 This is the fifth flowchart illustrating the underground exploration target inversion method in this application embodiment;

[0047] Figure 6 This is the sixth flowchart illustrating the underground exploration target inversion method in this application embodiment;

[0048] Figure 7 This is the seventh flowchart illustrating the underground exploration target inversion method in this application embodiment;

[0049] Figure 8 This is a structural diagram of the underground exploration target inversion device in the embodiments of this application;

[0050] Figure 9 This is a schematic diagram of the structure of the electronic device in the embodiments of this application.

[0051] Figure label:

[0052] 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 storage unit 9144, antenna 9111, speaker 9131, microphone 9132. Detailed Implementation

[0053] To make the objectives, technical solutions, and advantages of the embodiments of this application clearer, the technical solutions of the embodiments of this application will be clearly and completely described below with reference to the accompanying drawings. Obviously, the described embodiments are only some embodiments of this application, not all embodiments. Based on the embodiments of this application, all other embodiments obtained by those skilled in the art without creative effort are within the scope of protection of this application.

[0054] The acquisition, storage, use, and processing of data in this application all comply with the relevant provisions of national laws and regulations.

[0055] Considering the shortcomings of geophysical inversion, mainly focusing on the limitations and multiple interpretations of geophysical methods, how to improve the accuracy of interpretation results, and the challenges faced in the integration and application of new technologies, this application provides a method and apparatus for inverting underground exploration targets. By acquiring raw images from underground exploration remote sensing satellites, the method performs vertical radiometric operations on the raw images using a preset subatomic field generator to determine the corresponding vertical radiometric image of the target material and the dip and tilt angle of the target material. Based on the subatomic field generator and the tilt angle, the method performs radiometric operations on the raw images to determine the corresponding vertical dip angle radiometric image and parallel dip angle radiometric image of the target material. Based on the vertical dip angle radiometric image and the vertical radiometric image of the target material, the method determines the corresponding burial depth of the target material. Based on the parallel dip angle radiometric image of the target material, the method determines the corresponding thickness of the target material. Based on the burial depth and thickness of the target material, the method determines the corresponding target material inversion result. This improves the accuracy and efficiency of underground exploration inversion results based on subatomic radiation characteristics.

[0056] To improve the accuracy and efficiency of subsurface exploration inversion results based on subatomic radiation characteristics, this application provides an embodiment of a subsurface exploration target inversion method, see [link to embodiment]. Figure 1 The underground exploration target inversion method specifically includes the following:

[0057] Step S101: Obtain the original negative of the remote sensing satellite image of the underground exploration target, perform vertical radiation operation on the original negative according to the preset subatomic field generator, determine the vertical radiation image of the corresponding target material, and determine the trend and dip angle of the corresponding target material according to the vertical radiation image of the target material.

[0058] Optionally, in this embodiment, the purpose of this step is to process the original satellite image negative using subatomic properties to obtain a subatomic radiation image of the target material, providing a solid foundation for subsequently overcoming the multiple solutions in underground material inversion and improving the efficiency and accuracy of underground material inversion.

[0059] Understandably, by studying the correlation between the exploration target (solid mineral) and subatomic radiation spectrum information, the delineated anomaly distribution is the element (ore body) distribution. The element (ore body) anomaly is unique, unlike any existing inversion technology. The radiation image obtained based on subatomic characteristics is unique, effectively solving the problem of multiple solutions and low efficiency in underground material inversion.

[0060] Optionally, in this embodiment, the original negative of the remote sensing satellite image of the underground exploration target is acquired, and the original negative is subjected to vertical radiation operation according to a preset subatomic field generator to determine the corresponding vertical radiation image of the target material.

[0061] Specifically, in addition to the visible images of the Earth's surface, remote sensing satellite images also contain subatomic (lepton) fields of various geological bodies within the Earth that are invisible to the naked eye. In a radiochemistry laboratory, the raw satellite images are processed using a subatomic (lepton) field generator to apply a subatomic (lepton) field of its radiation frequency to the substance (mineral element) being tested. This generates subatomic (lepton) field resonance in the substance (mineral element), enhancing its radiation information intensity. This information is then developed on X-ray film, revealing the radiation information of the substance (mineral element) being tested. This radiation information is unique.

[0062] Specifically, vertical radiation refers to the subatomic field generator emitting a subatomic field at a 90° angle to the original film, so that the original film and the subatomic field generator form a subatomic field resonance.

[0063] Specifically, the principle of radiative resonance is that when leptons in a material body (such as rocks, ores, minerals, etc.) encounter energy fluctuations and resonate, they exhibit 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. Furthermore, when irradiated by a radiation source of a specific wavelength, the lepton field can absorb and re-emit radiant energy.

[0064] Since different substances have different subatomic field vibration frequencies, when extracting the subatomic resonance field, the vibration frequency of the subatomic field generator can be selected according to the vibration frequency of the target substance in the vibration frequency spectrum of different substances, and the subatomic distributed radiation resonance field can be obtained by irradiating remote sensing satellite images.

[0065] Next, the subatomic distributed radiation resonance field is projected onto a subatomic filter, and the target material radiation resonance is accurately extracted through the filter and the gel of the material to be retrieved arranged on the filter.

[0066] Optionally, in this embodiment, the subatomic filter can selectively filter radiation signals of specific wavelengths or energies, thereby extracting lepton radiation characteristics associated with the target material (such as an ore body). This allows for clearer identification of the target signal against a complex background. During data visualization, the subatomic filter can help generate clearer, more informative radiation images, enabling researchers to more intuitively understand the distribution and characteristics of the ore body.

[0067] Optionally, in this embodiment, the gel containing the substance to be retrieved can effectively concentrate the minerals or compounds in the target sample, facilitating subsequent analysis, especially the extraction of trace elements. It focuses on improving sample processing and detection sensitivity, and can be used in conjunction with techniques such as spectral analysis and chromatographic analysis to improve analytical efficiency and accuracy.

[0068] Understandably, after the above steps, the distributed radiation resonance field for the target mineral material is obtained.

[0069] Next, the radiation resonance of the target material is received by a preset photosensitive film to determine the corresponding radiation image of the target material.

[0070] Specifically, photographic film can respond to radiation energy. By irradiating a target material with resonant radiation, the photographic film can record these radiation signals. The selection of materials and processing methods for photographic film make it sensitive to subtle changes in radiation.

[0071] During the experiment, a pre-set radiation source (such as a laser or other high-energy radiation source) irradiates the photosensitive film. The purpose of this process is to enhance the signal, making the radiation characteristics of the target material more apparent. By using a suitable irradiation method, changes in radiation flux can be effectively recorded.

[0072] When photographic film receives a radiation signal, radiation resonance forms a corresponding image on the film. These images reflect the radiation characteristics of the target material, including radiation intensity and distribution patterns.

[0073] The entire radioactive experiment was conducted in three stages:

[0074] Satellite images are placed on the top layer, and the satellite images on the top layer are irradiated by an external subatomic field generator;

[0075] A subatomic filter is placed in the middle layer to receive the resonance field of the top layer. The accuracy of the target resonance field is improved by the filter and the gel of the substance to be retrieved.

[0076] The photosensitive film is placed at the bottom layer, and by setting a radiation source at the bottom of the photosensitive film, the resonant field can be effectively imaged.

[0077] Preferably, the photosensitive film can be X-ray film, and the radiation source below the photosensitive film can be an ultraviolet radiation source.

[0078] Understandably, the process of generating a vertical radiation image of a target material through radiation resonance involves multiple steps, including the principle of radiation resonance, the application of photosensitive materials, illumination procedures, and subsequent image processing. The successful implementation of this process provides a solid image foundation for subsequent target analysis and inversion.

[0079] Optionally, the orientation and tilt angle of the target material can be determined based on the vertical radiation image of the target material.

[0080] Specifically, after obtaining the vertical radiation image of the target material, it is necessary to obtain its contour anomaly map based on the image. This step can provide a basis for subsequent material inversion analysis.

[0081] It is understandable that the vertical radiation image of the target material is extracted based on the subatomic characteristics of the target material. Since the frequencies generated by subatomic resonance are different for each type of material, it can be determined that the vertical radiation image of the target material is unique and can reflect the true underground distribution of that target material.

[0082] Specifically, the process of obtaining the contour anomaly map from the image involves image enhancement of the vertical radiation image of the target material using a nonlinear algorithm.

[0083] More specifically, nonlinear algorithms are image nonlinear processing methods. They refer to the use of nonlinear mathematical operations and algorithms to process images, thereby improving image quality and visualization effects. Nonlinear processing includes the following key steps:

[0084] Image brightness and contrast adjustment: Through non-linear transformation, the brightness and contrast of the image are optimized to make the image of abnormal radiation intensity distribution clearer.

[0085] Noise Removal: Nonlinear filtering techniques are applied to remove noise from images and improve the overall image quality.

[0086] Feature description: Nonlinear image processing techniques are used for image edge detection, image segmentation, image enhancement, and image compression to better describe the features and structure in the image and improve the visual effect.

[0087] Specifically, secondly, the enhanced radiometric image is calibrated in planar position using a GIS (Geographic Information System) program. This process ensures that the extracted radiometric intensity image corresponds to the geographic coordinate system, guaranteeing the accuracy of the data's spatial location. Position calibration enables the correct location of radiometric anomalies within the actual geographic environment, thus providing a reliable geographic background for subsequent analysis.

[0088] Specifically, the final step involves using a geoscience vectorization program to vectorize the nonlinearly processed and calibrated images. This vectorization process converts raster images (pixel-based) into vector data (points, lines, and polygons), making the data more flexible and accurate for display and analysis. Vector data allows for more complex geological analyses and modeling; for example, it facilitates spatial analysis and overlay analysis, thus improving data usability.

[0089] As is understandable, vector data represents geographic information using points, lines, and polygons. For example, in mineral exploration, a radiation anomaly area in a mining region can be represented by a polygon, the boundary of which is formed by connecting multiple points (coordinates). Vector data typically has high accuracy because it uses coordinates to precisely locate specific geographic features.

[0090] As described above, by using a vector algorithm to perform vector transformation on the image after the planar position calibration operation, and determining the vector data of the image edge points, a vector graphic can be generated based on the vector data.

[0091] Next, by connecting all points with the same coordinates and vector markings, we can obtain the vertical radiation contour anomaly map corresponding to the vertical radiation image of the target material.

[0092] Specifically, the vertical radiation contour anomaly map obtained from the above steps is a planar map, but it will present ellipses of varying depths and sizes, linearly encircling each other, depending on the severity of the anomaly. A cross-section is cut at the peak of the central ellipse to restore the cross-sectional distribution characteristics of the vertical radiation map. At this point, the occurrence characteristics of the target material, namely the dip and dip angle of the target material, can be obtained based on the cross-sectional distribution characteristics.

[0093] The dip direction refers to the direction indicated by the projection of a line drawn perpendicular to the intersection of the bedding plane and the horizontal plane (strike line) downwards along the slope onto the horizontal plane. The dip direction indicates the direction in which the rock strata dip. The azimuth angle of the dip direction has only one direction, indicating the direction of the rock strata's dip.

[0094] Dip angle refers to the angle between the dip line on the bedding plane and its projection onto the horizontal plane; it is also called the true dip angle. The magnitude of the dip angle indicates the degree of inclination of the rock strata, and it varies between 0° and 90°.

[0095] Understandably, when measuring the attitude of rock strata, the dip direction and dip angle are usually recorded. These two parameters together can describe the spatial orientation of the rock strata.

[0096] For example, if an abnormal profile curve in a profile line shows a steep left branch and a gentle right branch, it indicates that the target body (ore body) dips to the right. The angle between the tangent to the right branch curve and the horizontal line is approximately the dip angle θ of the target body (ore body).

[0097] Through the above steps, the subatomic properties were successfully utilized to obtain a vertical radiation map through vertical radiation, solving the problem of multiple solutions in ore body inversion. Subsequently, the vertical radiation map was enhanced and vectorized using a digital method to obtain a contour map, making the vertical distribution of the ore body computable. Finally, the occurrence information of the ore body was determined based on the profile of the contour map, laying a solid information foundation for further ore body inversion.

[0098] Step S102: Perform a radiation operation on the original film according to the subatomic field generator and the tilt angle to determine the corresponding vertical tilt angle radiation image and the target material parallel tilt angle radiation image. Determine the corresponding burial depth of the target material according to the vertical tilt angle radiation image and the target material vertical radiation image. Determine the corresponding thickness of the target material according to the target material parallel tilt angle radiation image.

[0099] Optionally, the purpose of this step is to further irradiate the target material in multiple dimensions based on the above step S101 in order to determine more accurate structural information of the target material.

[0100] Optionally, in this embodiment, the original film is subjected to radiation operation based on the subatomic field generator and the tilt angle to determine the corresponding target material vertical tilt angle radiation image and target material parallel tilt angle radiation image.

[0101] Specifically, after obtaining the tilt angle of the target material, the directions along and perpendicular to the tilt angle are determined. The original film is then irradiated from these two directions using a subatomic field generator. The specific irradiation operation is the same as in step S101 and will not be repeated. Two more contour radiation images are obtained. At this point, three contour radiation images are obtained: image A (vertical radiation of the target material incident from the perpendicular direction), image B (vertical tilt angle radiation of the target material incident from the perpendicular tilt angle direction), and image C (parallel tilt angle radiation of the target material incident from the along the tilt angle direction), all obtained in step S101.

[0102] Optionally, in this embodiment, the burial depth of the target material is determined based on the vertical tilt radiation image of the target material and the vertical radiation image of the target material.

[0103] Specifically, the left vertex A1, right vertex A2, and center point O1 of the vertical radiation image of the target material;

[0104] The left vertex B1, right vertex B2, and center point O2 of the vertical tilt radiation image of the target material;

[0105] The left vertex C1, right vertex C2, and center point O3 of the parallel tilt angle radiation image of the target material;

[0106] Calculate the distance D1 between points A1 and B1 based on their actual coordinates. The burial depth of the ore body roof is H1 = D1 / tg(θ).

[0107] Calculate the distance D2 between points A2 and B2 based on their actual coordinates. The burial depth of the ore body bottom plate is H2 = D2 / tg(θ).

[0108] The distance D between points O1 and O2 is calculated based on their actual coordinates. The burial depth of the ore body center point is H = D / tg(θ).

[0109] As described above, based on the movement characteristics of the two radiation anomalies, the burial depth H1 of the top plate, the burial depth H of the center point, and the burial depth H2 of the bottom plate of the target body (ore body) can be determined.

[0110] Optionally, in this embodiment, the thickness of the target material is determined based on the parallel tilt angle radiation image of the target material.

[0111] Based on the distance D3 between the left vertex C1 and the right vertex C2 of the parallel tilt radiation image of the target material, the thickness T = D3 of the target body (ore body) can be roughly inferred.

[0112] The parallel tilt angle radiation image of the target material is obtained by directing light from the target material body along the tilt angle direction. The distance between the vertices of the resulting ellipse can be used to estimate the thickness of the ore body.

[0113] The specific technical solution is illustrated by examples from steps S101 and S102, as follows:

[0114] 1. In order to calculate the approximate depth range of the mineral deposit, subatomic (lepton) radiation is applied vertically to the original film to obtain a contour map of vertical radiation anomaly distribution. The dip and dip angle of the deep ore body reflected by the anomaly distribution contour map are then determined.

[0115] 2. Based on the dip angle of the ore body obtained in the first step, apply radiation on both sides of the vertical incident angle, one according to the dip angle of the ore body and the other according to the perpendicular to the dip angle of the ore body. The abnormal distribution of different radiation directions is obtained through the radiation in the three directions.

[0116] 3. Based on the geometric distribution pattern of radiation anomalies in three directions (translation of anomalies), calculate the characteristic parameters of the deposit: calculate the burial depth of the top, bottom, and center of the ore body by the geometric positional relationship between the radiation anomalies on the vertical undercarriage and the radiation anomalies at the dip angle of the ore body; infer the approximate thickness of the ore body by the radiation anomalies at the dip angle of the ore body.

[0117] Understandably, determining the occurrence and depth of a target body (ore body) by analyzing the distribution characteristics of radiation anomalies from different angles is simpler and more accurate, overcoming the limitations and multiple solutions of geophysical depth inversion calculations and improving the accuracy of the results.

[0118] Step S103: Perform target material inversion operation based on the target material burial depth and the target material thickness to determine the corresponding target material inversion result.

[0119] Optionally, in this embodiment, material inversion is mainly a process of inferring underground structures through inversion calculations using various physical data. It is primarily used for the detection of underground minerals, to help technicians understand the distribution of underground minerals, and to improve the utilization efficiency of underground minerals.

[0120] Optionally, in this embodiment, based on the occurrence information (dip, dip angle) and structural information (depth, thickness) of the underground target minerals obtained in steps S101 and S102, accurate inversion of the ore body can be achieved. At the same time, due to the uniqueness of the subatomic material, this method effectively overcomes the limitations and multiple solutions of data inversion depth calculation, and improves the accuracy and efficiency of data inversion depth calculation.

[0121] This example demonstrates how this embodiment utilizes subatomic properties to extract subatomic radiation maps for target material inversion, effectively overcoming the limitations and multiple solutions of data inversion depth calculation, and improving the accuracy and efficiency of data inversion depth calculation.

[0122] As described above, the underground exploration target inversion method provided in this application can determine the corresponding target material's vertical radiation image and the target material's dip and tilt angle by acquiring the original film of underground exploration remote sensing satellite imagery, performing vertical radiation operation on the original film using a preset subatomic field generator; performing radiation operation on the original film using the subatomic field generator and the tilt angle to determine the corresponding target material's vertical tilt angle radiation image and target material's parallel tilt angle radiation image; determining the corresponding target material's burial depth based on the target material's vertical tilt angle radiation image and target material's vertical radiation image; determining the corresponding target material's thickness based on the target material's parallel tilt angle radiation image; and determining the corresponding target material inversion result based on the target material's burial depth and target material thickness. This method improves the accuracy and efficiency of underground exploration inversion results based on subatomic radiation characteristics.

[0123] In one embodiment of the underground exploration target inversion method of this application, see [link to relevant documentation]. Figure 2 It can also specifically include the following:

[0124] Step S201: Perform digital processing on the vertical radiation image of the target material to determine the corresponding vertical radiation contour anomaly map;

[0125] Step S202: Perform a profile cutting operation on the vertical radiation contour anomaly map, and determine the tendency and dip angle of the corresponding target material based on the profile map obtained after the profile cutting operation.

[0126] Optionally, in this embodiment, the purpose of digitization is to locate and vectorize the target material image to facilitate calculation.

[0127] Optional digitization methods include non-linear algorithm enhancement, coordinate aiming, and vectorization.

[0128] Specifically, the process of obtaining the contour anomaly map from the image involves image enhancement of the vertical radiation image of the target material using a nonlinear algorithm.

[0129] More specifically, nonlinear algorithms are image nonlinear processing methods. They refer to the use of nonlinear mathematical operations and algorithms to process images, thereby improving image quality and visualization effects. Nonlinear processing includes the following key steps:

[0130] Image brightness and contrast adjustment: Through non-linear transformation, the brightness and contrast of the image are optimized to make the image of abnormal radiation intensity distribution clearer.

[0131] Noise Removal: Nonlinear filtering techniques are applied to remove noise from images and improve the overall image quality.

[0132] Feature description: Nonlinear image processing techniques are used for image edge detection, image segmentation, image enhancement, and image compression to better describe the features and structure in the image and improve the visual effect.

[0133] Specifically, secondly, the enhanced radiometric image is calibrated in planar position using a GIS (Geographic Information System) program. This process ensures that the extracted radiometric intensity image corresponds to the geographic coordinate system, guaranteeing the accuracy of the data's spatial location. Position calibration enables the correct location of radiometric anomalies within the actual geographic environment, thus providing a reliable geographic background for subsequent analysis.

[0134] Specifically, the final step involves using a geoscience vectorization program to vectorize the nonlinearly processed and calibrated images. This vectorization process converts raster images (pixel-based) into vector data (points, lines, and polygons), making the data more flexible and accurate for display and analysis. Vector data allows for more complex geological analyses and modeling; for example, it facilitates spatial analysis and overlay analysis, thus improving data usability.

[0135] As is understandable, vector data represents geographic information using points, lines, and polygons. For example, in mineral exploration, a radiation anomaly area in a mining region can be represented by a polygon, the boundary of which is formed by connecting multiple points (coordinates). Vector data typically has high accuracy because it uses coordinates to precisely locate specific geographic features.

[0136] As described above, by using a vector algorithm to perform vector transformation on the image after the planar position calibration operation, and determining the vector data of the image edge points, a vector graphic can be generated based on the vector data.

[0137] Next, by connecting all points with the same coordinates and vector markings, we can obtain the vertical radiation contour anomaly map corresponding to the vertical radiation image of the target material.

[0138] Specifically, the vertical radiation contour anomaly map obtained from the above steps is a planar map, but it will present ellipses of varying depths and sizes, linearly encircling each other, depending on the severity of the anomaly. A cross-section is cut at the peak of the central ellipse to restore the cross-sectional distribution characteristics of the vertical radiation map. At this point, the occurrence characteristics of the target material, namely the dip and dip angle of the target material, can be obtained based on the cross-sectional distribution characteristics.

[0139] The dip direction refers to the direction indicated by the projection of a line drawn perpendicular to the intersection of the bedding plane and the horizontal plane (strike line) downwards along the slope onto the horizontal plane. The dip direction indicates the direction in which the rock strata dip. The azimuth angle of the dip direction has only one direction, indicating the direction of the rock strata's dip.

[0140] Dip angle refers to the angle between the dip line on the bedding plane and its projection onto the horizontal plane; it is also called the true dip angle. The magnitude of the dip angle indicates the degree of inclination of the rock strata, and it varies between 0° and 90°.

[0141] Understandably, when measuring the attitude of rock strata, the dip direction and dip angle are usually recorded. These two parameters together can describe the spatial orientation of the rock strata.

[0142] For example, if an abnormal profile curve in a profile line shows a steep left branch and a gentle right branch, it indicates that the target body (ore body) dips to the right. The angle between the tangent to the right branch curve and the horizontal line is approximately the dip angle θ of the target body (ore body).

[0143] Through step S202, this embodiment successfully utilized subatomic properties to obtain a vertical radiation map through vertical radiation, solving the problem of multiple solutions in ore body inversion. Subsequently, the vertical radiation map was enhanced and vectorized using a digital method to obtain a contour map, making the vertical distribution of the ore body computable. Finally, the occurrence information of the ore body was determined based on the profile of the contour map, laying a solid information foundation for further ore body inversion.

[0144] In one embodiment of the underground exploration target inversion method of this application, see [link to relevant documentation]. Figure 3 It can also specifically include the following:

[0145] Step S301: Determine the corresponding vertical tilt direction and parallel tilt direction based on the tilt angle;

[0146] Step S302: Perform radiation operations on the original film from the vertical tilt direction and the parallel tilt direction respectively according to the subatomic field generator to determine the corresponding vertical tilt radiation image and parallel tilt radiation image of the target material.

[0147] Optionally, in this embodiment, after obtaining the tilt angle of the target material, the direction along the tilt angle and the direction perpendicular to the tilt angle are determined respectively. The original film is then irradiated from these two directions using a subatomic field generator. The specific irradiation operation is the same as in step S101 and will not be described in detail. Two more contour radiation images can be obtained. At this point, three contour radiation images are obtained, namely, the target material vertical radiation image A obtained from the vertical direction, the target material vertical tilt angle radiation image B obtained from the direction perpendicular to the tilt angle, and the target material parallel tilt angle radiation image C obtained from the direction along the tilt angle.

[0148] Through step S302, this embodiment obtains a multi-directional radiation map, laying the image foundation for subsequent material inversion.

[0149] In one embodiment of the underground exploration target inversion method of this application, see [link to relevant documentation]. Figure 4 It can also specifically include the following:

[0150] Step S401: Determine the burial depth of the top plate of the target material based on the distance between the left vertex of the vertical tilt radiation image of the target material and the angle of the tilt angle;

[0151] Step S402: Determine the burial depth of the target material's center point based on the distance between the center point of the vertical tilt radiation image of the target material and the angle of the tilt.

[0152] Step S403: Determine the corresponding burial depth of the target material base plate based on the distance between the right vertex of the vertical tilt radiation image of the target material and the angle of the tilt angle;

[0153] Step S404: Determine the corresponding target material burial depth based on the top burial depth of the target material, the center point burial depth of the target material, and the bottom burial depth of the target material.

[0154] Optionally, in this embodiment, the left vertex A1, right vertex A2, and center point O1 of the vertical radiation image of the target material;

[0155] The left vertex B1, right vertex B2, and center point O2 of the vertical tilt radiation image of the target material;

[0156] The left vertex C1, right vertex C2, and center point O3 of the parallel tilt angle radiation image of the target material;

[0157] Calculate the distance D1 between points A1 and B1 based on their actual coordinates. The burial depth of the ore body roof is H1 = D1 / tg(θ).

[0158] Calculate the distance D2 between points A2 and B2 based on their actual coordinates. The burial depth of the ore body bottom plate is H2 = D2 / tg(θ).

[0159] The distance D between points O1 and O2 is calculated based on their actual coordinates. The burial depth of the ore body center point is H = D / tg(θ).

[0160] As described above, based on the movement characteristics of the two radiation anomalies, the burial depth H1 of the top plate, the burial depth H of the center point, and the burial depth H2 of the bottom plate of the target body (ore body) can be determined.

[0161] Through step S404, this embodiment successfully calculated the burial depth of the underground target mineral and obtained the top burial depth, center burial depth and floor burial depth of the mineral, thus determining the burial depth attribute of the mineral.

[0162] In one embodiment of the underground exploration target inversion method of this application, see [link to relevant documentation]. Figure 5 It can also specifically include the following:

[0163] Step S501: Determine the left and right vertices of the target material's parallel tilt angle radiation image based on the target material's parallel tilt angle radiation image;

[0164] Step S502: Determine the corresponding target material thickness based on the straight-line distance between the left and right vertices.

[0165] Optionally, in this embodiment, the thickness T = D3 of the target body (ore body) can be roughly inferred from the distance D3 between the left vertex C1 and the right vertex C2 of the parallel tilt angle radiation image of the target material.

[0166] The parallel tilt angle radiation image of the target material is obtained by directing light from the target material body along the tilt angle direction. The distance between the vertices of the resulting ellipse can be used to estimate the thickness of the ore body.

[0167] Through step S502, this embodiment successfully calculated the thickness of the underground target mineral and determined the thickness attribute of the mineral.

[0168] In one embodiment of the underground exploration target inversion method of this application, see [link to relevant documentation]. Figure 6 It can also specifically include the following:

[0169] Step S601: Perform image enhancement processing on the vertical radiation image of the target material according to a nonlinear image processing algorithm to determine the corresponding enhanced radiation image;

[0170] Step S602: Perform digital processing on the enhanced image according to preset geographic coordinates and preset vector algorithm to determine the corresponding vertical radiation contour anomaly map.

[0171] Optionally, in this embodiment, the nonlinear algorithm is an image nonlinear processing method, which refers to processing images by employing nonlinear mathematical operations and algorithms to improve image quality and visualization effects. Nonlinear processing includes the following key steps:

[0172] Image brightness and contrast adjustment: Through non-linear transformation, the brightness and contrast of the image are optimized to make the image of abnormal radiation intensity distribution clearer.

[0173] Noise Removal: Nonlinear filtering techniques are applied to remove noise from images and improve the overall image quality.

[0174] Feature description: Nonlinear image processing techniques are used for image edge detection, image segmentation, image enhancement, and image compression to better describe the features and structure in the image and improve the visual effect.

[0175] Optionally, in this embodiment, a GIS (Geographic Information System) program is used to perform planar position calibration on the nonlinearly enhanced radiation image. This process ensures that the extracted radiation intensity image corresponds to the geographic coordinate system, ensuring the accuracy of the spatial location of the data. Through position calibration, radiation anomalies can be correctly located in the actual geographic environment, thereby providing a reliable geographic background for subsequent analysis.

[0176] Specifically, a geoscience vectorization program is used to vectorize the nonlinearly processed and calibrated images. This vectorization process converts raster images (pixel-based) into vector data (points, lines, and polygons), making the data more flexible and accurate in display and analysis. Vector data allows for more complex geological analysis and modeling; for example, it makes spatial analysis and overlay analysis easier, thus improving data usability.

[0177] Through step S602, this embodiment successfully performs nonlinear enhancement, coordinate calibration, and vectorization on the radiation image, enabling the radiation image to be used for calculations and laying the foundation for subsequent physical inversion.

[0178] In one embodiment of the underground exploration target inversion method of this application, see [link to relevant documentation]. Figure 7 It can also specifically include the following:

[0179] Step S701: Perform vertical irradiation on the original film according to the subatomic field emitted by the preset subatomic field generator, which has the same radiation frequency as the target material;

[0180] Step S702: Receive the subatomic field radiation resonance obtained after the vertical radiation operation according to the preset subatomic filter, and perform a filtering operation on the subatomic field radiation resonance to determine the corresponding target material vertical radiation resonance.

[0181] Step S703: Receive the vertical radiation resonance of the target material according to the preset photosensitive film, and determine the corresponding vertical radiation image of the target material.

[0182] Optionally, in this embodiment, in addition to the visible Earth surface image, remote sensing satellite images also contain subatomic (lepton) fields of various geological bodies within the Earth that are invisible to the naked eye. In a radiochemistry laboratory, the raw satellite image negatives are processed using a subatomic (lepton) field generator to apply a subatomic (lepton) field of its radiation frequency to the substance (mineral element) being tested. This generates subatomic (lepton) field resonance in the substance (mineral element) being tested, enhancing its radiation information intensity. This information is then developed on X-ray film, thus revealing the radiation information of the substance (mineral element) being tested. This radiation information is unique.

[0183] Specifically, vertical radiation refers to the subatomic field generator emitting a subatomic field at a 90° angle to the original film, so that the original film and the subatomic field generator form a subatomic field resonance.

[0184] Since different substances have different subatomic field vibration frequencies, when extracting the subatomic resonance field, the vibration frequency of the subatomic field generator can be selected according to the vibration frequency of the target substance in the vibration frequency spectrum of different substances, and the subatomic distributed radiation resonance field can be obtained by irradiating remote sensing satellite images.

[0185] Next, the subatomic distributed radiation resonance field is projected onto a subatomic filter, and the target material radiation resonance is accurately extracted through the filter and the gel of the material to be retrieved arranged on the filter.

[0186] Optionally, in this embodiment, the subatomic filter can selectively filter radiation signals of specific wavelengths or energies, thereby extracting lepton radiation characteristics associated with the target material (such as an ore body). This allows for clearer identification of the target signal against a complex background. During data visualization, the subatomic filter can help generate clearer, more informative radiation images, enabling researchers to more intuitively understand the distribution and characteristics of the ore body.

[0187] Optionally, in this embodiment, the gel containing the substance to be retrieved can effectively concentrate the minerals or compounds in the target sample, facilitating subsequent analysis, especially the extraction of trace elements. It focuses on improving sample processing and detection sensitivity, and can be used in conjunction with techniques such as spectral analysis and chromatographic analysis to improve analytical efficiency and accuracy.

[0188] Understandably, after the above steps, the distributed radiation resonance field for the target mineral material is obtained.

[0189] Next, the radiation resonance of the target material is received by a preset photosensitive film to determine the corresponding radiation image of the target material.

[0190] Specifically, photographic film can respond to radiation energy. By irradiating a target material with resonant radiation, the photographic film can record these radiation signals. The selection of materials and processing methods for photographic film make it sensitive to subtle changes in radiation.

[0191] During the experiment, a pre-set radiation source (such as a laser or other high-energy radiation source) irradiates the photosensitive film. The purpose of this process is to enhance the signal, making the radiation characteristics of the target material more apparent. By using a suitable irradiation method, changes in radiation flux can be effectively recorded.

[0192] When photographic film receives a radiation signal, radiation resonance forms a corresponding image on the film. These images reflect the radiation characteristics of the target material, including radiation intensity and distribution patterns.

[0193] The entire radioactive experiment was conducted in three stages:

[0194] Satellite images are placed on the top layer, and the satellite images on the top layer are irradiated by an external subatomic field generator;

[0195] A subatomic filter is placed in the middle layer to receive the resonance field of the top layer. The accuracy of the target resonance field is improved by the filter and the gel of the substance to be retrieved.

[0196] The photosensitive film is placed at the bottom layer, and by setting a radiation source at the bottom of the photosensitive film, the resonant field can be effectively imaged.

[0197] Preferably, the photosensitive film can be X-ray film, and the radiation source below the photosensitive film can be an ultraviolet radiation source.

[0198] Through step S703, this embodiment successfully utilizes multiple steps, including the principle of radiation resonance, the application of photosensitive materials, illumination operations, and subsequent image processing, to provide a solid image foundation for subsequent target analysis and inversion.

[0199] To improve the accuracy and efficiency of subatomic radiation-based inversion results, this application provides an embodiment of a subsurface exploration target inversion device for implementing all or part of the aforementioned subsurface exploration target inversion method. See [link to embodiment]. Figure 8 The underground exploration target inversion device specifically includes the following components:

[0200] The target material occurrence determination module 10 is used to acquire the original film of remote sensing satellite image of underground exploration target, perform vertical radiation operation on the original film according to the preset subatomic field generator, determine the corresponding target material vertical radiation image, and determine the corresponding target material dip and dip angle according to the target material vertical radiation image.

[0201] The target material morphology determination module 20 is used to perform radiation operation on the original film according to the subatomic field generator and the tilt angle, determine the corresponding target material vertical tilt angle radiation image and target material parallel tilt angle radiation image, determine the corresponding target material burial depth according to the target material vertical tilt angle radiation image and target material vertical radiation image, and determine the corresponding target material thickness according to the target material parallel tilt angle radiation image.

[0202] The target material inversion module 30 is used to perform target material inversion operations based on the burial depth and thickness of the target material, and determine the corresponding target material inversion results.

[0203] As described above, the underground exploration target inversion device provided in this application embodiment can acquire the original film of underground exploration remote sensing satellite imagery, perform vertical radiation operation on the original film according to a preset subatomic field generator, determine the corresponding target material's vertical radiation image and the target material's dip and tilt angle; perform radiation operation on the original film according to the subatomic field generator and the tilt angle to determine the corresponding target material's vertical tilt angle radiation image and target material's parallel tilt angle radiation image; determine the corresponding target material's burial depth according to the target material's vertical tilt angle radiation image and target material's vertical radiation image; determine the corresponding target material's thickness according to the target material's parallel tilt angle radiation image; and determine the corresponding target material inversion result according to the target material's burial depth and target material thickness. This improves the accuracy and efficiency of underground exploration inversion results based on subatomic radiation characteristics.

[0204] From a hardware perspective, in order to improve the accuracy and efficiency of underground exploration inversion results based on subatomic radiation characteristics, this application provides an embodiment of an electronic device for implementing all or part of the underground exploration target inversion method, wherein the electronic device specifically includes the following:

[0205] The system comprises a processor, memory, a communications interface, and a bus; wherein the processor, memory, and communications interface communicate with each other via the bus; the communications interface is used to realize information transmission between the underground exploration target inversion method and core business systems, user terminals, and related databases and other related devices; the logic controller can be a desktop computer, tablet computer, or mobile terminal, etc., and this embodiment is not limited to these. In this embodiment, the logic controller can be implemented with reference to the embodiments of the underground exploration target inversion method in the present embodiment, and the contents of the embodiments of the underground exploration target inversion method are incorporated herein, and repeated parts will not be described again.

[0206] It is understood that the user terminal may include smartphones, tablet computers, network set-top boxes, portable computers, desktop computers, personal digital assistants (PDAs), in-vehicle devices, smart wearable devices, etc. Among these, the smart wearable devices may include smart glasses, smartwatches, smart bracelets, etc.

[0207] In practical applications, parts of the underground exploration target inversion method can be executed on the electronic device side as described above, or all operations can be completed in the client device. The choice can be made based on the processing power of the client device and the limitations of the user's usage scenario. This application does not impose any limitations on this. If all operations are completed in the client device, the client device may further include a processor.

[0208] The aforementioned client device may have a communication module (i.e., a communication unit) that can communicate with a remote server to achieve data transmission. The server may include a server on the task scheduling center side; in other implementation scenarios, it 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, a server cluster consisting of multiple servers, or a distributed server structure.

[0209] Figure 9 This is a schematic block diagram illustrating the system configuration of the electronic device 9600 according to an embodiment of this application. Figure 9 As shown, the electronic device 9600 may include a central processing unit 9100 and a memory 9140; the memory 9140 is coupled to the central processing unit 9100. It is worth noting that... Figure 9 This is an example; other types of structures can also be used to supplement or replace this structure to achieve telecommunications functions or other functions.

[0210] In one embodiment, the underground exploration target inversion method function can be integrated into the central processing unit 9100. The central processing unit 9100 can be configured to perform the following control:

[0211] Step S101: Obtain the original negative of the remote sensing satellite image of the underground exploration target, perform vertical radiation operation on the original negative according to the preset subatomic field generator, determine the vertical radiation image of the corresponding target material, and determine the trend and dip angle of the corresponding target material according to the vertical radiation image of the target material.

[0212] Step S102: Perform a radiation operation on the original film according to the subatomic field generator and the tilt angle to determine the corresponding vertical tilt angle radiation image and the target material parallel tilt angle radiation image. Determine the corresponding burial depth of the target material according to the vertical tilt angle radiation image and the target material vertical radiation image. Determine the corresponding thickness of the target material according to the target material parallel tilt angle radiation image.

[0213] Step S103: Perform target material inversion operation based on the target material burial depth and the target material thickness to determine the corresponding target material inversion result.

[0214] As described above, the electronic device provided in this application acquires the original film of a remote sensing satellite image for underground exploration. It then performs vertical radiometric operation on the original film using a preset subatomic field generator to determine the corresponding vertical radiometric image of the target material and the dip and tilt angle of the target material. Based on the subatomic field generator and the tilt angle, it performs radiometric operation on the original film to determine the corresponding vertical tilt radiometric image and parallel tilt radiometric image of the target material. Based on the vertical tilt radiometric image and the vertical radiometric image of the target material, it determines the corresponding burial depth of the target material. Based on the parallel tilt radiometric image of the target material, it determines the corresponding thickness of the target material. Based on the burial depth and thickness of the target material, it determines the corresponding target material inversion result. This improves the accuracy and efficiency of underground exploration inversion results based on subatomic radiation characteristics.

[0215] In another embodiment, the underground exploration target inversion method can be configured separately from the central processing unit 9100. For example, the underground exploration target inversion method can be configured as a chip connected to the central processing unit 9100, and the underground exploration target inversion method function can be realized through the control of the central processing unit.

[0216] like Figure 9 As shown, the electronic device 9600 may further 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 need to include these components. Figure 9 All components shown; in addition, the electronic device 9600 may also include Figure 9 For components not shown, please refer to existing technologies.

[0217] like Figure 9 As shown, the central processing unit 9100, sometimes also referred to as a controller or operating control, may include a microprocessor or other processor device and / or logic device, which receives inputs and controls the operation of various components of the electronic device 9600.

[0218] The memory 9140 may be, for example, one or more of a cache, flash memory, hard drive, removable media, volatile memory, non-volatile memory, or other suitable devices. It may store the aforementioned failure-related information, and also store a program for executing that information. The central processing unit 9100 may execute the program stored in the memory 9140 to perform information storage or processing, etc.

[0219] Input unit 9120 provides input to central processing unit 9100. Input unit 9120 may be, for example, a keypad or touch input device. Power supply 9170 provides power to electronic device 9600. Display 9160 displays images and text. Display may be, for example, an LCD display, but is not limited thereto.

[0220] The memory 9140 can be a solid-state memory, such as a read-only memory (ROM), random access memory (RAM), a SIM card, etc. It can also be a memory that retains information even when power is off, can be selectively erased, and contains more data; examples of this type of memory are sometimes referred to as EPROMs. The memory 9140 can 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 for storing application programs and function programs or processes for executing the operation of the electronic device 9600 via the central processing unit 9100.

[0221] 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 the electronic device's communication functions and / or for performing other functions of the electronic device (such as messaging applications, address book applications, etc.).

[0222] 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 processing unit 9100 to provide input signals and receive output signals, which is the same as in a conventional mobile communication terminal.

[0223] Based on different communication technologies, multiple communication modules 9110 can be configured in the same electronic device, such as cellular network modules, Bluetooth modules, and / or wireless LAN modules. The communication module 9110 is also coupled to a speaker 9131 and a microphone 9132 via an audio processor 9130 to provide audio output via the speaker 9131 and receive audio input from the microphone 9132, thereby realizing typical telecommunications functions. The audio processor 9130 may include any suitable buffer, decoder, amplifier, etc. Furthermore, the audio processor 9130 is also coupled to a central processing unit 9100, enabling on-device recording via the microphone 9132 and on-device playback of stored sound via the speaker 9131.

[0224] Embodiments of this application also provide a computer-readable storage medium capable of implementing all steps of the underground exploration target inversion method with a server or client as the execution subject in the above embodiments. The computer-readable storage medium stores a computer program that, when executed by a processor, implements all steps of the underground exploration target inversion method with a server or client as the execution subject in the above embodiments. For example, when the processor executes the computer program, it implements the following steps:

[0225] Step S101: Obtain the original negative of the remote sensing satellite image of the underground exploration target, perform vertical radiation operation on the original negative according to the preset subatomic field generator, determine the vertical radiation image of the corresponding target material, and determine the trend and dip angle of the corresponding target material according to the vertical radiation image of the target material.

[0226] Step S102: Perform a radiation operation on the original film according to the subatomic field generator and the tilt angle to determine the corresponding vertical tilt angle radiation image and the target material parallel tilt angle radiation image. Determine the corresponding burial depth of the target material according to the vertical tilt angle radiation image and the target material vertical radiation image. Determine the corresponding thickness of the target material according to the target material parallel tilt angle radiation image.

[0227] Step S103: Perform target material inversion operation based on the target material burial depth and the target material thickness to determine the corresponding target material inversion result.

[0228] As described above, the computer-readable storage medium provided in this application embodiment acquires the original film of underground exploration remote sensing satellite images, performs vertical radiometric operation on the original film using a preset subatomic field generator, determines the corresponding vertical radiometric image of the target material and the dip and tilt angle of the target material; performs radiometric operation on the original film using the subatomic field generator and the tilt angle to determine the corresponding vertical tilt radiometric image and parallel tilt radiometric image of the target material; determines the corresponding burial depth of the target material based on the vertical tilt radiometric image and the vertical radiometric image of the target material; determines the corresponding thickness of the target material based on the parallel tilt radiometric image of the target material; and determines the corresponding target material inversion result based on the burial depth and the thickness of the target material. This improves the accuracy and efficiency of underground exploration inversion results based on subatomic radiation characteristics.

[0229] Embodiments of this application also provide a computer program product capable of implementing all steps in the underground exploration target inversion method described above, where the execution subject is a server or client. When executed by a processor, this computer program / instruction implements the steps of the underground exploration target inversion method. For example, the computer program / instruction implements the following steps:

[0230] Step S101: Obtain the original negative of the remote sensing satellite image of the underground exploration target, perform vertical radiation operation on the original negative according to the preset subatomic field generator, determine the vertical radiation image of the corresponding target material, and determine the trend and dip angle of the corresponding target material according to the vertical radiation image of the target material.

[0231] Step S102: Perform a radiation operation on the original film according to the subatomic field generator and the tilt angle to determine the corresponding vertical tilt angle radiation image and the target material parallel tilt angle radiation image. Determine the corresponding burial depth of the target material according to the vertical tilt angle radiation image and the target material vertical radiation image. Determine the corresponding thickness of the target material according to the target material parallel tilt angle radiation image.

[0232] Step S103: Perform target material inversion operation based on the target material burial depth and the target material thickness to determine the corresponding target material inversion result.

[0233] As described above, the computer program product provided in this application acquires the original film of a remote sensing satellite image for underground exploration. It then performs vertical radiometric operation on the original film using a preset subatomic field generator to determine the corresponding vertical radiometric image of the target material and the dip and tilt angle of the target material. Based on the subatomic field generator and the tilt angle, it performs radiometric operation on the original film to determine the corresponding vertical tilt radiometric image and parallel tilt radiometric image of the target material. Based on the vertical tilt radiometric image and the vertical radiometric image of the target material, it determines the corresponding burial depth of the target material. Based on the parallel tilt radiometric image of the target material, it determines the corresponding thickness of the target material. Based on the burial depth and thickness of the target material, it determines the corresponding target material inversion result. This improves the accuracy and efficiency of underground exploration inversion results based on subatomic radiation characteristics.

[0234] Those skilled in the art will understand that embodiments of the present invention can be provided as methods, apparatus, or computer program products. Therefore, the present invention can take the form of a completely hardware embodiment, a completely software embodiment, or an embodiment combining software and hardware aspects. Furthermore, the present invention can take the form of a computer program product embodied 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.

[0235] This invention is described with reference to flowchart illustrations and / or block diagrams of methods, apparatus (devices), and computer program products according to embodiments of the invention. It will be understood that each block of the flowchart illustrations and / or block diagrams, and combinations of blocks in the flowchart illustrations and / or block diagrams, can be implemented by computer program instructions. These computer program instructions can be provided to a processor of a general-purpose computer, special-purpose computer, embedded processor, or other programmable data processing apparatus to produce a machine, such that the instructions, which execute via the processor of the computer or other programmable data processing apparatus, generate instructions for implementing the flowchart illustrations and / or block diagrams. Figure 1 One or more processes and / or boxes Figure 1 A device that provides the functions specified in one or more boxes.

[0236] These computer program instructions may also be stored in a computer-readable storage medium that can direct a computer or other programmable data processing device to function in a particular manner, such that the instructions stored in the computer-readable storage medium produce an article of manufacture including instruction means, which are implemented in a process Figure 1 One or more processes and / or boxes Figure 1 The function specified in one or more boxes.

[0237] These computer program instructions may also be loaded onto a computer or other programmable data processing equipment to cause a series of operational steps to be performed on the computer or other programmable equipment to produce a computer-implemented process, thereby providing instructions that execute on the computer or other programmable equipment for implementing the process. Figure 1 One or more processes and / or boxes Figure 1 The steps of the function specified in one or more boxes.

[0238] Specific embodiments have been used to illustrate the principles and implementation methods of this invention. The descriptions of the embodiments above are only for the purpose of helping to understand the method and core ideas of this invention. At the same time, for those skilled in the art, there will be changes in the specific implementation methods and application scope based on the ideas of this invention. Therefore, the content of this specification should not be construed as a limitation of this invention.

Claims

1. A method for inverting underground exploration targets, characterized in that, The method includes: The original negative of remote sensing satellite image of underground exploration target is acquired. The original negative is subjected to vertical radiometric operation according to a preset subatomic field generator to determine the vertical radiometric image of the target material. The dip and tilt angle of the target material are determined according to the vertical radiometric image of the target material. The original film is irradiated using the subatomic field generator and the tilt angle to determine the corresponding vertical tilt angle irradiation image and the target material parallel tilt angle irradiation image. The target material burial depth is determined based on the target material vertical tilt angle irradiation image and the target material vertical irradiation image. The target material thickness is determined based on the target material parallel tilt angle irradiation image. Based on the burial depth and thickness of the target material, a target material inversion operation is performed to determine the corresponding target material inversion result.

2. The underground exploration target inversion method according to claim 1, characterized in that, The step of determining the dip and tilt angle of the target material based on the vertical radiation image of the target material includes: The vertical radiation image of the target material is digitally processed to determine the corresponding vertical radiation contour anomaly map. The vertical radiation contour anomaly map is subjected to a profile cutting operation, and the tendency and dip angle of the corresponding target material are determined based on the profile map obtained after the profile cutting operation.

3. The underground exploration target inversion method according to claim 1, characterized in that, The step of performing a radiation operation on the original film based on the subatomic field generator and the tilt angle to determine the corresponding vertical tilt angle radiation image and parallel tilt angle radiation image of the target material includes: The corresponding vertical tilt direction and parallel tilt direction are determined based on the tilt angle. The subatomic field generator performs radiation operations on the original film from the vertical tilt direction and the parallel tilt direction respectively to determine the corresponding vertical tilt radiation image and parallel tilt radiation image of the target material.

4. The underground exploration target inversion method according to claim 1, characterized in that, The step of determining the corresponding burial depth of the target material based on the vertical tilt radiation image of the target material and the vertical radiation image of the target material includes: The burial depth of the top plate of the target material is determined based on the distance between the left vertices of the vertical tilt radiation image of the target material and the angle of the tilt. The burial depth of the target material's center point is determined based on the distance between the center points of the vertical tilt radiation images of the target material and the angle of the tilt. The corresponding burial depth of the target material's base plate is determined based on the distance between the right vertices of the vertical tilt radiation image of the target material and the angle of the tilt. The corresponding target material burial depth is determined based on the burial depth of the top plate of the target material, the burial depth of the center point of the target material, and the burial depth of the bottom plate of the target material.

5. The underground exploration target inversion method according to claim 1, characterized in that, Determining the thickness of the target material based on the parallel tilt angle radiometric image of the target material includes: The left and right vertices of the target material's parallel tilt angle radiation image are determined based on the target material's parallel tilt angle radiation image. The thickness of the target material is determined based on the straight-line distance between the left and right vertices.

6. The method for inverting underground exploration targets according to claim 2, characterized in that, The step of digitally processing the vertical radiation image of the target material to determine the corresponding vertical radiation contour anomaly map includes: The vertical radiation image of the target material is enhanced using a nonlinear image processing algorithm to determine the corresponding enhanced radiation image. The enhanced image is digitally processed based on preset geographic coordinates and a preset vector algorithm to determine the corresponding vertical radiation contour anomaly map.

7. The method for inverting underground exploration targets according to claim 1, characterized in that, The step of performing vertical radiation operation on the original film according to a preset subatomic field generator to determine the corresponding vertical radiation image of the target material includes: The original film is subjected to vertical radiation operation based on a subatomic field emitted by a preset subatomic field generator that has the same radiation frequency as the target material. The subatomic field radiation resonance obtained after the vertical radiation operation is received by a preset subatomic filter, and the subatomic field radiation resonance is filtered to determine the corresponding target material vertical radiation resonance. Based on the vertical radiation resonance of the target material received by the preset photosensitive film, the corresponding vertical radiation image of the target material is determined.

8. A device for inverting underground exploration targets, characterized in that, The device includes: The target material occurrence determination module is used to acquire the original negative of remote sensing satellite images of underground exploration targets, perform vertical radiation operation on the original negative according to a preset subatomic field generator, determine the corresponding target material vertical radiation image, and determine the dip and dip angle of the target material according to the target material vertical radiation image. The target material morphology determination module is used to perform radiation operation on the original film according to the subatomic field generator and the tilt angle, determine the corresponding target material vertical tilt angle radiation image and target material parallel tilt angle radiation image, determine the corresponding target material burial depth according to the target material vertical tilt angle radiation image and target material vertical radiation image, and determine the corresponding target material thickness according to the target material parallel tilt angle radiation image; The target material inversion module is used to perform target material inversion operations based on the burial depth and thickness of the target material, and determine the corresponding target material inversion results.

9. An electronic device comprising a memory, a processor, and a computer program stored in the memory and executable on the processor, characterized in that, When the processor executes the program, it implements the steps of the underground exploration target inversion method according to any one of claims 1 to 7.

10. A computer-readable storage medium having a computer program stored thereon, characterized in that, When executed by a processor, the computer program implements the steps of the underground exploration target inversion method according to any one of claims 1 to 7.

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