Geological profile map encryption method and system
By performing telescopic encryption transformation of the drilling spacing, hole depth and layered thickness in the geological profile, and encrypting the identification and labeling information, the problem that traditional encryption forms cannot ensure data confidentiality and verification requirements at the same time, achieving high data security and retention of key attribute information.
Patent Information
- Application Number
- CN202510053734.4
- Authority / Receiving Office
- CN · China
- Patent Type
- Applications(China)
- Current Assignee / Owner
- Filing Date
- 2025-01-14
- Publication Date
- 2025-06-20
AI Technical Summary
During the geological profile trading process, traditional encryption forms cannot ensure the confidentiality of data and user inspection needs at the same time, and cannot effectively protect the core data in the geological profile drawing.
The drilling spacing, hole depth and layer thickness in the geological profile are encrypted by telescopic encryption transformation method, and the identification and annotation information is encrypted to generate the final encrypted geological profile.
Through encryption processing, we ensure that the core data of the geological profile picture is not leaked, which improves the security of the data. At the same time, we retain key attribute information, so that users can understand the profile picture overview and meet the verification needs before transactions.
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Figure CN120180485A_ABST
Abstract
Description
Technical Field
[0001] The present invention relates to the technical field of engineering geology, and particularly to a method and system for encrypting geological section maps. Background Art
[0002] By trading existing geological data of enterprises online through a network platform, the value-added of existing geological data can be realized. During the process of trading geological section maps through an online platform, it is necessary to judge whether the data meets the user's needs through data display. How to ensure the confidentiality of data during the display process is an important issue. The traditional encryption form of geological section maps mainly encrypts files, such as encrypting CAD or PDF files, etc. The encrypted data cannot be displayed and cannot meet the inspection needs of the buyer before the transaction. Therefore, it is necessary to study a method for encrypting the content of geological section maps to ensure that there is no leakage during the display process, while at the same time retaining key attribute information for users to understand the general situation of the section map. Summary of the Invention
[0003] This application provides a method and system for encrypting geological section maps to solve the problem of encrypting geological section maps during the trading process and at the same time retaining key attribute information for users to understand the general situation of the section map.
[0004] According to a first aspect, in one embodiment, a method for encrypting a geological section map is provided, and the method includes:
[0005] Step S1, obtaining a geological section map, where the geological section map contains formation stratification information of different boreholes;
[0006] Step S2, performing telescopic encryption transformation on the borehole spacing, borehole depth, and formation layer thickness included in the geological section map;
[0007] Step S3, encrypting the identification and marking information included in the geological section map to obtain the finally encrypted geological section map.
[0008] Further, the step S1 specifically includes:
[0009] Obtaining single-point formation information through field exploration, and obtaining a geological section map through the projection of exploration points and connecting layers of formation lines.
[0010] Further, the step S2 specifically includes:
[0011] Performing telescopic encryption transformation on the borehole spacing, including the following steps:
[0012] Calculating the horizontal spacing between adjacent boreholes on the section map, and arranging them in sequence to form a borehole spacing matrix x1:
[0013]
[0014] where n is the number of drill holes;
[0015] Generate a random encryption matrix A for the horizontal spacing of drill holes using a random number generation algorithm:
[0016]
[0017] Perform a linear stretching or compression transformation on the drill hole spacing using the random encryption matrix A, that is, obtain the stretched and compressed drill hole spacing matrix x2 by calculating the Hadamard product of the random matrix A and the drill hole spacing matrix x1:
[0018]
[0019] Update the drill hole spacing in the geological section diagram according to the values in the stretched and compressed drill hole spacing matrix x2.
[0020] Furthermore, the specific steps of step S2 include:
[0021] Perform a stretching and encryption transformation on the drill hole depths, including the following steps:
[0022] Record all the drill hole depths on the geological section diagram as matrix x3:
[0023]
[0024] where n is the number of drill holes;
[0025] Generate a random encryption matrix B for the drill hole depths using a random number generation algorithm:
[0026]
[0027] Correct the drill hole depths using the random encryption matrix B, and the corrected drill hole depths of all drill holes are:
[0028]
[0029] Record the stratigraphic layer depths of the i-th drill hole as:
[0030]
[0031] m is the number of stratigraphic layers of the i-th drill hole;
[0032] Modify the stratigraphic layer depths of the i-th drill hole using the i-th element of matrix B, and the modified stratigraphic layer depths of the i-th drill hole are:
[0033]
[0034] Then sequentially modify the stratigraphic layer depths of all drill holes on the section diagram to obtain the modified stratigraphic depths.
[0035] Further, step S2 specifically includes:
[0036] Performing telescopic encryption transformation on the drilling layer thickness, including the following steps:
[0037] For any drilling hole i on the modified geological section diagram, record the matrix of formation thicknesses on the drilling hole as:
[0038]
[0039] where m is the number of formation layers of drilling hole i;
[0040] Using a random number generation algorithm to generate a random encryption matrix C for the formation thicknesses of each drilling hole i :
[0041]
[0042] Using the random encryption matrix C i and the formation thickness matrix dchd i Calculating the Hadamard product to obtain the encrypted formation thickness:
[0043]
[0044] Then, successively encrypt the layer thicknesses of all drilling holes to obtain a geological section diagram with randomly encrypted formation thicknesses.
[0045] Further, step S2 specifically further includes:
[0046] Correcting the inter-hole formation line, including:
[0047] For the lenticular formation, using the hole depth correction coefficient corresponding to the drilling holes connected to the lenticular formation in the random encryption matrix B to modify the depth of the lenticular formation nodes located between the drilling holes, thereby obtaining a modified lenticular formation line.
[0048] Further, step S2 specifically further includes:
[0049] Correcting the inter-hole formation line, including:
[0050] For the lenticular formation, first calculate the average value of the top depth and the bottom depth of the lenticular formation, and then take the average value as the annihilation depth of the lenticular formation.
[0051] Further, step S2 specifically further includes:
[0052] Correcting the inter-hole formation line, including:
[0053] For the annihilation stratum, first determine on which stratum line the stratum annihilation body is annihilated, and denote the corresponding stratum line as L. Then, vertically move the annihilation stratum nodes between the drill holes up and down so that the corresponding annihilation stratum nodes fall on the stratum line L, thereby obtaining the corrected annihilation stratum line.
[0054] Further, step S3 specifically includes:
[0055] Delete the remaining identification and annotation information on the cross-sectional view except for the basic information, thereby obtaining the finally encrypted geological cross-sectional view. The basic information includes drill holes, stratum boundaries, stratum patterns, and stratum descriptions.
[0056] According to a second aspect, an embodiment provides a geological cross-sectional view encryption system, and the system includes:
[0057] A geological cross-section acquisition module for acquiring a geological cross-sectional view, where the geological cross-sectional view contains stratum stratification information of different drill holes;
[0058] An encryption processing module for performing stretching and encryption transformation on the drill hole spacing, drill hole depth, and drill hole stratification thickness included in the geological cross-sectional view;
[0059] An identification and annotation information processing module for encrypting the identification and annotation information included in the geological cross-sectional view to obtain the finally encrypted geological cross-sectional view.
[0060] The present application provides a geological cross-sectional view encryption method and system, which have the following beneficial effects:
[0061] (1) For the method for encrypting the content of the geological cross-sectional view proposed by the present invention, since all information such as the actual stratification position and horizontal spacing of all strata are false information after encryption, it ensures that the core data of the strata will not be leaked, significantly improves the security during the display or transmission of the geological cross-sectional view, and avoids data leakage.
[0062] (2) When using the encrypted geological cross-sectional view of the present invention for display, on the premise of avoiding data leakage during the display of the geological cross-sectional view, the encrypted data should also be able to reflect the basic characteristics of the geological cross-sectional view. The buyer can clearly understand the detailed degree of the content of the cross-sectional view and the general stratum situation of the site, so that the buyer can judge whether the data meets the requirements. Description of the Drawings
[0063] Figure 1 It is a flowchart of a geological cross-sectional view encryption method provided by an embodiment of the present invention;
[0064] Figure 2 It is a specific implementation flowchart of a geological cross-sectional view encryption method provided by an embodiment of the present invention;
[0065] Figure 3 An example geological cross-section diagram in a geological cross-section diagram encryption method provided by an embodiment of the present invention;
[0066] Figure 4 The geological cross-section diagram after encryption of the horizontal spacing of boreholes in a geological cross-section diagram encryption method provided by an embodiment of the present invention;
[0067] Figure 5 The geological cross-section diagram after encryption and correction of the hole depth in a geological cross-section diagram encryption method provided by an embodiment of the present invention;
[0068] Figure 6 The geological cross-section diagram after lens body correction in a geological cross-section diagram encryption method provided by an embodiment of the present invention;
[0069] Figure 7 Comparison of partial enlarged views before and after correction of the annihilated formation in a geological cross-section diagram encryption method provided by an embodiment of the present invention;
[0070] Figure 8 The geological cross-section diagram after lens body correction and formation annihilation correction in a geological cross-section diagram encryption method provided by an embodiment of the present invention;
[0071] Figure 9 The geological cross-section diagram after encryption and correction of the formation thickness in a geological cross-section diagram encryption method provided by an embodiment of the present invention;
[0072] Figure 10 The geological cross-section diagram after lens body correction in a geological cross-section diagram encryption method provided by an embodiment of the present invention;
[0073] Figure 11 The geological cross-section diagram after correction of the formation annihilation boundary in a geological cross-section diagram encryption method provided by an embodiment of the present invention;
[0074] Figure 12 Schematic diagram of the logical structure of a geological cross-section diagram encryption system provided by an embodiment of the present invention. Detailed implementation manners
[0075] The present invention will be further described in detail below in conjunction with the specific embodiments and the accompanying drawings. Similar elements in different embodiments are denoted by related similar element numbers. In the following embodiments, many detailed descriptions are provided to enable a better understanding of the present application. However, those skilled in the art can easily recognize that some of the features can be omitted in different situations, or can be replaced by other elements, materials, or methods. In some cases, some operations related to the present application are not shown or described in the specification, which is to avoid the core part of the present application being overwhelmed by excessive descriptions. For those skilled in the art, it is not necessary to describe these related operations in detail, and they can fully understand the related operations based on the descriptions in the specification and the general technical knowledge in the art.
[0076] In addition, the features, operations, or characteristics described in the specification can be combined in any suitable manner to form various embodiments. At the same time, the steps or actions in the method description can also be reordered or adjusted in an obvious manner by those skilled in the art. Therefore, the various sequences in the specification and the drawings are only for clearly describing a certain embodiment, and do not mean that they are the necessary sequences, unless it is stated that a certain sequence must be followed.
[0077] The first embodiment of the present invention provides a method for densifying a geological cross-section diagram. The following will be described in detail in conjunction with Figure 1 and Figure 2 for detailed description.
[0078] As Figure 1 shown, in step S1, a geological cross-section diagram is obtained, and the geological cross-section diagram contains the formation stratification information of different boreholes.
[0079] Specifically, there are various methods for obtaining the geological cross-section diagram data, such as hand-drawing, using professional software to draw, collecting other cross-section diagram materials, etc. Regardless of which data acquisition method is used, the most original data source is: obtaining single-point formation information through field exploration, and obtaining the geological cross-section diagram through the projection of exploration points and connecting layers of formation lines.
[0080] As Figure 1 shown, in step S2, stretching and densifying transformation is performed on the borehole spacing, borehole depth, and borehole layer thickness included in the geological cross-section diagram.
[0081] The above steps specifically include:
[0082] Step S21, performing stretching and densifying transformation on the borehole spacing, including the following steps:
[0083] Calculate the horizontal spacing between adjacent boreholes on the cross-section diagram, and arrange them in sequence to form a borehole spacing matrix x1:
[0084]
[0085] where n is the number of boreholes;
[0086] Generate a random encryption matrix A for the horizontal spacing of boreholes using a random number generation algorithm:
[0087]
[0088] Perform a linear stretching or compression transformation on the borehole spacing using the random encryption matrix A, that is, obtain the stretched or compressed borehole spacing matrix x2 by calculating the Hadamard product of the random matrix A and the borehole spacing matrix x1:
[0089]
[0090] Update the borehole spacing in the geological section diagram according to the values in the stretched or compressed borehole spacing matrix x2.
[0091] As Figure 3 shown, this example geological section diagram has a total of three boreholes ZK1, ZK2, and ZK3, and the horizontal spacings of the boreholes are 39 and 40 respectively, denoted as Figure 3 There are a total of three boreholes, and there are 2 spacings between adjacent boreholes. Therefore, the generated random matrix contains 2 data, and the generated random matrix All data in matrix A are in the range (0, 2). Using to Figure 3 stretch or compress the borehole spacing. The original borehole spacing is The Hadamard product (multiplying the data at corresponding positions) of the two matrices is calculated to obtain the stretched borehole spacing After transformation, as Figure 4 shown.
[0092] Step S22: Perform a stretching and encryption transformation on the borehole depth, including the following steps:
[0093] Record the depths of all boreholes on the geological section diagram as matrix x3:
[0094]
[0095] where n is the number of boreholes;
[0096] Generate a random encryption matrix B for the borehole depth using a random number generation algorithm. The random matrix B has 1 column and n rows:
[0097]
[0098] Correct the borehole depths using the random encryption matrix B. After correction, the depths of all boreholes are:
[0099]
[0100] Denote the depth of each stratum layer of the \(i\)-th borehole as follows:
[0101]
[0102] \(m\) is the number of stratum layers of the \(i\)-th borehole;
[0103] Modify the depth of the \(i\)-th borehole using the \(i\)-th element of matrix \(B\). After modification, the depths of each layer of the \(i\)-th borehole are:
[0104]
[0105] Then, modify the depths of all borehole layers on the cross-section diagram in sequence to obtain the modified stratum depth. Figure 4 In the example geological cross-section diagram, there are a total of 3 boreholes, and there are a total of three elements in the generated random matrix \(B\). Example geological cross-section diagram borehole depth Using the random matrix Modified borehole depth The depth of the ZK1 layer is shendu1 = Using The first data 1.2 for correction, after correction The depth of the ZK2 layer is Using The second data 0.9 for correction, after correction The depth of the ZK3 layer is Using The third data 1.2 for correction, after correction The cross-section diagram after the scaling transformation is as Figure 5 shown.
[0106] Step S23, correction of the inter-borehole stratum line. The inter-borehole stratum nodes are divided into two categories: lenticular stratum nodes and annihilation stratum nodes. The closed stratum area formed by the connection of the stratum line with a single borehole is defined as a lenticle. The intersection of the stratum line with other stratum lines between boreholes is defined as stratum annihilation.
[0107] (1) For the lenticular stratum, use the borehole depth correction coefficient corresponding to the lenticular stratum in the randomly encrypted matrix \(B\) of the borehole connected to the lenticular stratum to modify the depth of the lenticular stratum nodes located between the boreholes, and obtain the modified lenticular stratum line.
[0108] As Figure 5 shown in, the karst stratum of ZK2 is a lenticle, and the stratum nodes 1 and 2 marked with red circles are the lenticle nodes to be scaled and transformed. From Figure 4The initial buried depths of Node 1 and Node 2 are 30 and 30 respectively. After being corrected by the depth correction coefficient of 0.9 for ZK2, the buried depths become 27 and 27. The cross-sectional view after the lens body correction is as Figure 6 shown.
[0109] (2) For the annihilated formation, first determine which formation line the formation annihilation body annihilates on, and record the corresponding formation line as L1. Then, vertically move the annihilated formation nodes between the boreholes up and down so that the corresponding annihilated formation nodes fall on the formation line L1, thereby obtaining the corrected annihilated formation line.
[0110] As Figure 5 shown, the node 3 marked by the red circle in it is the formation annihilation point. From Figure 4 it can be seen that this formation line was originally annihilated on the upper formation line. Therefore, vertically move this annihilation node so that the annihilation node falls on this formation line again, thereby obtaining the corrected formation line of the annihilation body. The partial enlarged views before and after the correction of the annihilated formation are shown in Figure 7 . The geological cross-sectional view after the lens body correction and the annihilated formation correction is shown in Figure 8 .
[0111] Step S24, perform stretching, densifying, and transformation on the layer thickness of the boreholes, including the following steps:
[0112] For any borehole i on the modified geological cross-sectional view, record the matrix of the layer thicknesses of each formation on the borehole as:
[0113]
[0114] where m is the number of formation layers of borehole i;
[0115] Use the random number generation algorithm to generate the random densifying matrix C i of the layer thicknesses of each formation of the borehole:
[0116]
[0117] Use the random densifying matrix C i and the layer thickness matrix dchd i to calculate the Hadamard product to obtain the densified layer thickness:
[0118]
[0119] Then, sequentially densify the layer thicknesses of all boreholes to obtain the geological cross-sectional view with randomly densified layer thicknesses.
[0120] Figure 8 In for ZK1, record the layer thickness from top to bottom, For ZK3, record the formation thickness from top to bottom. The corrected geological cross-section is as Figure 9 shown.
[0121] Step S25, re-correction of the inter-borehole formation line.
[0122] (1) For the lenticular formation, first calculate the average of the top depth and the bottom depth of the lenticular formation, and then take the average value as the annihilation depth of the lenticular formation.
[0123] Figure 9 In, the karst cave of ZK2 is a lenticle, the top depth is 24.93, the bottom depth is 26.73, and the average value is (24.93 + 26.73) / 2 = 25.8. Thus, the annihilation depth of the lenticle is corrected to 25.8, and the corrected geological cross-section is Figure 10 .
[0124] (2) For the annihilated formation, first determine which formation line the formation annihilation body annihilates on, and record the corresponding formation line as L2. Then, vertically move the annihilated formation nodes between the boreholes up and down so that the corresponding annihilated formation nodes fall on the formation line L2, thereby obtaining the corrected annihilated formation line.
[0125] Figure 9 In, the gravel soil formation line is annihilated upward and annihilates on the formation boundary between the silty clay and the limestone. Therefore, Figure 10 In, the annihilated formation nodes are vertically moved downward to the formation boundary between the silty clay and the limestone to obtain the corrected geological cross-section of the annihilated formation.
[0126] As Figure 1 shown, in step S3, the identification annotation information included in the geological cross-section is encrypted to obtain the final encrypted geological cross-section.
[0127] Specifically, in addition to the boreholes, formation boundaries, formation patterns, and formation descriptions on the cross-section, it also includes the water level line, in-situ test markings, sampling symbol markings, weathering line markings, etc. Except for the boreholes, formation boundaries, formation patterns, and formation descriptions, other information on the cross-section is deleted. Thus, the final encrypted geological cross-section is obtained.
[0128] In the above example cross-section, for the convenience of demonstration, there are no information markings such as sampling symbols, water level lines, and weathering lines. Therefore Figure 11 is the final encrypted geological cross-section.
[0129] In addition, it should be noted that the present invention can use any random number generation algorithm to generate random numbers; and the representation methods of each matrix in the present invention can be replaced by any other symbols, and the above symbols are only used for the convenience of explaining the logical relationship.
[0130] Corresponding to the geological section drawing encryption method disclosed above, an embodiment of the present invention also discloses a geological section drawing encryption system, as Figure 12 shown, which specifically includes:
[0131] A geological section obtaining module, configured to obtain a geological section drawing, where the geological section drawing contains formation stratification information of different drill holes;
[0132] An encryption processing module, configured to perform telescopic encryption transformation on the drill hole spacing, drill hole depth, and drill hole stratification thickness included in the geological section drawing;
[0133] An identification annotation information processing module, configured to perform encryption processing on the identification annotation information included in the geological section drawing to obtain a finally encrypted geological section drawing.
[0134] It should be noted that for a detailed description of the geological section drawing encryption system provided by the embodiment of the present invention, reference can be made to the relevant description of the geological section drawing encryption method provided by the embodiment of the present application, which will not be elaborated here.
[0135] In addition, an embodiment of the present invention also provides an electronic device, where the device includes: a processor and a memory; the memory is used to store one or more program instructions; the processor is used to run one or more program instructions to execute the steps of the geological section drawing encryption method described in any one of the above.
[0136] It should be noted that for a detailed description of the electronic device provided by the embodiment of the present invention, reference can be made to the relevant description of the geological section drawing encryption method provided by the embodiment of the present application, which will not be elaborated here.
[0137] In addition, an embodiment of the present invention also provides a computer-readable storage medium, where a computer program is stored on the computer-readable storage medium, and when the computer program is executed by a processor, the steps of the geological section drawing encryption method described in any one of the above are implemented.
[0138] It should be noted that for a detailed description of the computer-readable storage medium provided by the embodiment of the present invention, reference can be made to the relevant description of the geological section drawing encryption method provided by the embodiment of the present application, which will not be elaborated here.
[0139] Those skilled in the art can understand that all or part of the functions of the various methods in the above embodiments can be implemented in a hardware manner or in a computer program manner. When all or part of the functions in the above embodiments are implemented in a computer program manner, the program can be stored in a computer-readable storage medium. The storage medium can include: read-only memory, random access memory, magnetic disk, optical disk, hard disk, etc. The above functions can be realized by a computer executing the program. For example, the program is stored in the memory of the device, and when the processor executes the program in the memory, the above all or part of the functions can be realized. In addition, when all or part of the functions in the above embodiments are implemented in a computer program manner, the program can also be stored in a storage medium such as a server, another computer, magnetic disk, optical disk, flash drive or mobile hard disk, and saved to the memory of the local device by downloading or copying, or the system of the local device is updated. When the processor executes the program in the memory, all or part of the functions in the above embodiments can be realized.
[0140] The above uses specific examples to elaborate on the present invention, which is only used to help understand the present invention and is not intended to limit the present invention. For those skilled in the art of the present invention, according to the idea of the present invention, several simple deductions, deformations or substitutions can also be made.
Claims
1. A geological profile encryption method, characterized in that: The method comprises: Step S1, obtaining a geological profile, wherein the geological profile contains stratigraphic information of different boreholes; Step S2, performing telescopic and densification transformation on the borehole spacing, borehole depth and borehole layer thickness contained in the geological profile; Step S3, encrypting the identification information contained in the geological profile to obtain a final encrypted geological profile.
2. A geological profile encryption method according to claim 1, characterized in that: The step S1 specifically includes: Single-point stratigraphic information is obtained through field exploration, and geological profiles are obtained through the projection of exploration points and the connection of stratigraphic lines.
3. A geological profile encryption method according to claim 1, characterized in that: The step S2 specifically includes: The drilling spacing is expanded and encrypted, including the following steps: Calculate the horizontal spacing between adjacent boreholes on the profile diagram and arrange them in order to form a borehole spacing matrix x1: Where n is the number of holes drilled; A random number generation algorithm is used to generate a random encryption matrix A of the horizontal spacing of the boreholes: The random encryption matrix A is used to perform linear stretching or compression transformation on the borehole spacing, that is, by calculating the Hadamard product of the random matrix A and the borehole spacing matrix x1, the borehole spacing matrix x2 after the stretching transformation is obtained: The borehole spacing in the geological profile is updated according to the values in the borehole spacing matrix x2 after the scaling transformation.
4. A geological profile encryption method as claimed in claim 3, characterized in that: The step S2 specifically includes: The drilling hole depth is expanded and expanded, and the following steps are included: The depths of all boreholes on the geological profile are recorded as matrix x3: Where n is the number of holes drilled; A random number generation algorithm is used to generate a random encryption matrix B of the drilling depth: The random encryption matrix B is used to correct the drilling depth. After correction, the depth of all drilling holes is: The depth of each stratum layer of the i-th borehole is recorded as: m is the number of stratigraphic layers in the ith borehole; The i-th element of matrix B is used to modify the layer depth of the i-th drilling hole. After modification, the layer depths of the i-th drilling hole are: Then, the stratified depths of all the boreholes on the profile are modified in turn to obtain the modified stratum depths.
5. A geological profile encryption method as claimed in claim 4, characterized in that: The step S2 specifically includes: The drilling layer thickness is expanded and contracted, and the density transformation is performed, including the following steps: For any borehole i on the modified geological profile, the thickness matrix of each stratum on the borehole is recorded as: Where m is the number of stratigraphic layers in borehole i; The random number generation algorithm is used to generate the random encryption matrix C of the thickness of each stratum in the borehole i : Using random encryption matrix C i and the formation thickness matrix dchd i Calculate the Hadamard product to get the thickness of the densified stratum: Then the layer thickness of all the boreholes is encrypted in turn to obtain a geological profile with randomly encrypted layer thickness.
6. A geological profile encryption method as claimed in claim 4, characterized in that: The step S2 specifically includes: Correction of the stratigraphic lines between holes, including: For the lens formation, the hole depth correction coefficient corresponding to the borehole connected to the lens formation in the random encryption matrix B is used to modify the depth of the lens formation node between the boreholes to obtain the modified lens formation line.
7. A geological profile encryption method according to claim 5, characterized in that: The step S2 specifically includes: Correction of the stratigraphic lines between holes, including: For the lens formation, the average value of the top depth and the bottom depth of the lens formation is first calculated, and then the annihilation depth of the lens formation is taken as the average value.
8. A geological profile encryption method as claimed in claim 4 or 5, characterized in that: The step S2 specifically includes: Correction of the stratigraphic lines between holes, including: For the annihilation formation, first determine on which formation line the formation annihilation body is annihilated, record the corresponding formation line as L, and then vertically move the annihilation formation nodes located between the boreholes up and down so that the corresponding annihilation formation nodes fall on the formation line L, thereby obtaining the corrected annihilation formation line.
9. A geological profile encryption method according to claim 1, characterized in that: The step S3 specifically includes: The remaining identification and annotation information on the profile map except the basic information is deleted, thereby obtaining the final encrypted geological profile map, wherein the basic information includes boreholes, stratigraphic boundaries, stratigraphic patterns, and stratigraphic descriptions.
10. A geological profile encryption system, characterized in that: The system comprises: A geological profile acquisition module, used to acquire a geological profile map, wherein the geological profile map contains stratigraphic information of different boreholes; An encryption processing module, used for performing telescopic encryption transformation on the borehole spacing, borehole depth and borehole layer thickness contained in the geological profile; The identification and annotation information processing module is used to encrypt the identification and annotation information contained in the geological profile to obtain the final encrypted geological profile.