CN107180452A - The stratified geological objects modeling method of the multi-source data coupling on the stratum containing standard - Google Patents

The stratified geological objects modeling method of the multi-source data coupling on the stratum containing standard Download PDF

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CN107180452A
CN107180452A CN201710310068.3A CN201710310068A CN107180452A CN 107180452 A CN107180452 A CN 107180452A CN 201710310068 A CN201710310068 A CN 201710310068A CN 107180452 A CN107180452 A CN 107180452A
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stratum
drilling
source data
modeling
formation beds
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吴信才
万波
吴亮
周顺平
胡茂胜
杨林
叶亚琴
余国宏
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BEIJING ZONDY CYBER TECHNOLOGY CO LTD
Shenzhen China Land Software Engineering Co Ltd
WUHAN ZONDY CYBER CO Ltd
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BEIJING ZONDY CYBER TECHNOLOGY CO LTD
Shenzhen China Land Software Engineering Co Ltd
WUHAN ZONDY CYBER CO Ltd
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    • G06COMPUTING; CALCULATING OR COUNTING
    • G06TIMAGE DATA PROCESSING OR GENERATION, IN GENERAL
    • G06T17/00Three dimensional [3D] modelling, e.g. data description of 3D objects
    • G06T17/30Polynomial surface description
    • GPHYSICS
    • G06COMPUTING; CALCULATING OR COUNTING
    • G06FELECTRIC DIGITAL DATA PROCESSING
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Abstract

The present invention relates to Geologic modeling field, the stratified geological objects modeling method of the multi-source data coupling on especially a kind of stratum containing standard, its difference is:It comprises the following steps:A) selection modeling region, extracts multi-source data and is coupled;B) step a) is used to build the regional stratum sequence table for covering whole modeling region;C) the aspect sequence number on all stratum contained in each drilling is determined;D) the generation triangulation network forms the aspect on each stratum;E) row interpolation is entered to the aspect elevation on each stratum of generation in step d), with the aspect on smooth each stratum;F) formation beds after step e) processing are subjected to intersecting processing, and adjust stratum elevation;G) triangulation network of neighbouring formation beds is sutured on vertical, constitutes complete three-dimensional geological physical model.The present invention comes in various data constraints, sufficiently make use of existing data source, and modeling result more coincide with actual conditions, and accuracy is higher.

Description

The stratified geological objects modeling method of the multi-source data coupling on the stratum containing standard
Technical field
The present invention relates to Review of geologic model building techniques field, the multi-source data coupling on especially a kind of stratum containing standard is layeredly Plastid modeling method.
Background technology
The concept of three-dimensional geological modeling is earliest by Canadian Simon W Houlding in proposition in 1994, its main work( Can be by computer and visualization technique, under three-dimensional environment, by spatial information management, GEOLOGICAL INTERPRETATION, spatial analysis and pre- The instruments such as survey, soil statistics, physical contents analysis and graph visualization combine, and understanding, table are removed in digitized form Geologic body and geological environment are reached and reproduced, the Three-dimensional Display and geological analysis of geological model is realized.Compared to traditional presentation of information Mode, the boundary condition and geologic body that three dimension strata model can express complicated geological phenomenon complete and accurate include variously Texture is made, and dynamic three-dimensional display effect is realistically presented.It is aided with powerful interactive space analysis tool, three dimension strata model again Three-dimensional geological entity can be flexibly and comfortably showed, strengthens the intuitive and accuracy of geological analysis to greatest extent.
The transition of evolution and stratum by history, some depth from earth's surface to underground, stratum has a phase To stable order up and down, it is standard stratum that this, which is thus referred to as,.Standard stratum reflects era change rule, the lithology on stratum Changing rule and depositional environment.For complicated geologic body, such as basement rock exposure area, structure development region, stratum is merely capable of The parameter information on reference standard stratum, the syntople up and down on stratum can not comply fully with the requirement on standard stratum.
Multi-source data includes:It is borehole data, cross-sectional data, isopleth data, geology panel data, exploration line data, disconnected The construction data such as layer.Wherein, drilling is the columnar three-dimensional body with narrow and small surface area and certain depth, and engineering drilling method is to obtain Take the important method of the three-dimensional spatial informations such as underground rock-soil layer distribution situation, construction, water content.Drill hole information is directly perceived, accurate, detailed Thin characteristic also makes it have vital meaning in three-dimensional formation simulation;Profile includes drill hole information and expertise Knowledge, is a more complicated class in whole modelling data source, introduces crossing section data and can determine ground in modeling region Layer skeleton;Isopleth data must have correct Height attribute, and it reflects the rolling shape of single stratal surface;Geological map The distribution that can reflect between subsurface formations and various geological structures and staggered case;The construction data such as tomography are mainly derived from Geophysical interpretation data, its introducing can increase the complexity of modeling.
Current modeling method, data source is single, the reaction actual conditions that the model of foundation can only be unilateral, lacks for this Fall into, the invention provides a kind of simple stratified geological objects three-dimensional geological modeling method based on the coupling of the multi-source datas such as drilling.
The content of the invention
Coupled it is an object of the invention to the shortcoming for overcoming prior art there is provided a kind of multi-source data on stratum containing standard Stratified geological objects modeling method, various data constraints are come in, and sufficiently make use of existing data source, modeling result and reality Situation is more coincide, and accuracy is higher.
To solve above technical problem, the technical scheme is that:The stratiform of the multi-source data coupling on the stratum containing standard Geological modeling method, its difference is:It comprises the following steps:
A) selection modeling region, extracts multi-source data and is coupled;
B) borehole data in the multi-source data of step a) extractions is used to build the regional stratum layer for covering whole modeling region Sequence table;
C) each drilling in the modeling region is compareed with the regional stratum sequence table respectively, it is determined that each The aspect sequence number on contained all stratum in drilling;
D) on the basis of all drilling orifice coordinates included in each stratum, with reference to modeling regional boundary condition, using three The angle subdivision algorithm generation triangulation network forms the aspect on each stratum;
E) the aspect elevation on each stratum of generation in step d) is inserted with the multi-source data that coupling is extracted through step a) Value, with the aspect on smooth each stratum;
F) formation beds after step e) processing are subjected to intersecting processing, and stratum elevation is adjusted according to the sequence on stratum;
G) triangulation network of neighbouring formation beds is sutured on vertical, constitutes complete three-dimensional geological entity mould Type.
By above technical scheme, the specific method for extracting multi-source data in step a) and being coupled is:S1 multi-source) is extracted Data;S2) by step s1) in extract multi-source data be converted into three-dimensional geological key element;S3) to step s2) in three-dimensional geological Key element is coupled, and forms ground particle key element and geology line feature.
By above technical scheme, the specific method that the regional stratum sequence table is built in step b) is:Built described in traversal All drilling in mould region, picks out and discloses a most drilling of rock stratum information, and using its formation information as first Beginning stratigraphic sequence table, is then compared initial stratigraphic sequence table with residue drilling one by one, if both sequences are inconsistent, update step Sequence table, if both sequences are consistent, skips Present Borehole, continues more next drilling, so repeatedly, and generation one, which is covered, builds The regional stratum sequence table on mould region whole stratum.
By above technical scheme, the specific side of the aspect sequence number on all stratum contained in each drilling is determined in step c) Method is:Drilling top formation beds are numbered, corresponding numbering in regional stratum sequence table is then used in from top to bottom To determine the numbering of the formation beds of the bottom surface on each stratum in drilling, and ignore in the drilling of present collation non-existently Numbering corresponding to layer.
By above technical scheme, row interpolation is entered using Kriging regression method in step e), its specific method is:Extract respectively The elevation information at each formation beds control point, the elevation of each unknown point in formation beds is obtained with the control point interpolation Value;If the point in formation beds is consistent with the coordinate drilled, interpolation is not needed.
By above technical scheme, the method for the intersecting processing of formation beds is in step f):Using based on AABB-OBB borders Collision detection algorithm, to the formation beds triangulation network carry out collision detection, comprise the following steps that:
Y1 the AABB detections storehouse that formation beds) are built in units of single formation beds is detected, N number of stratum is built altogether The AABB detections storehouse in face, wherein N is the stratum number of plies contained in the modeling region;
It just can be regarded as two AABB when y2) only having projections of two AABB in three reference axis to have overlapping to intersect, accordingly To the AABB between n-th of AABB detection storehouse and other AABB detections storehouse to being compared, intersecting AABB pairs is found out, n's is first Initial value is 1, if not intersecting between two AABB pairs of formation beds, and the triangle for constituting formation beds is also impossible to phase Hand over;
Y3 intersecting AABB pairs) is blown, OBB detections storehouse is set up in units of triangle and carries out collision detection, correspondence is found out OBB in intersect triangle pair;
Y4 more accurate positioning intersection algorithm) is carried out to intersecting triangle, judges that whether it intersects, and obtain friendship really Point;
Y5 the triangle that is detected in the aspect of understratum) is deleted, using step y4) in the intersection point that calculates be used as new control It is processed, triangulation is re-started to understratum aspect;
Y6) judge whether to have traveled through all formation beds, if not having, return to step y2) restart circulation, if It has been compared that, then intersect processing and complete.
By above technical scheme, the specific method of adjustment stratum elevation is in step f):It is a certain in some formation beds Point TriPnti, the point TriPntiHeight value be Zi, point TriPnt can be retrievediWith the corresponding points in a upper formation beds TriPnti-1, the point TriPnti-1Height value be Zi-1If, ZiMore than Zi-1, then by ZiAgain it is entered as Zi-1
Prior art is contrasted, beneficial features of the invention are:The layered geology of the multi-source data coupling on the stratum containing standard In volume modeling method, there is topological relation determine, unanimous between the higher and lower levels between each formation beds, can greatly simplify follow-up The complexity of processing, strengthens the robustness of algorithm;Various data constraints are come in, existing data source is sufficiently make use of, builds Mould result and actual conditions are more coincide, and accuracy is higher, particularly stratal pinch-outs drilling, lenticular body, layer interlayer etc. The control of complicated geological phenomenon.
Brief description of the drawings
Fig. 1 is schematic flow sheet of the embodiment of the present invention;
Fig. 2 is extracted with coupling schematic flow sheet for multi-source data in the embodiment of the present invention;
Fig. 3 is the intersecting processing schematic flow sheet of formation beds in the embodiment of the present invention.
Embodiment
To make the object, technical solutions and advantages of the present invention clearer, below in conjunction with attached in the embodiment of the present invention Figure, the technical scheme in the embodiment of the present invention is clearly and completely described.It should be appreciated that being retouched below with reference to accompanying drawing The embodiment stated is exemplary, is only used for explaining the present invention, and is not considered as limiting the invention.
The embodiments of the invention provide a kind of simple stratified geological objects three-dimensional geological based on the coupling of the multi-source datas such as drilling Modeling method.Various data constraints are come in, existing data source is sufficiently make use of, modeling result is more kissed with actual conditions Close, accuracy is higher, particularly stratal pinch-outs drilling, lenticular body, the complicated geological phenomenon such as layer interlayer control.
It refer to Fig. 1, the stratified geological objects modeling method of the multi-source data coupling on stratum containing standard of the embodiment of the present invention, its Comprise the following steps:
Step a), selection modeling region, extract multi-source data and are coupled., may for specific modeling region There is substantial amounts of geological information, these information are although various, but it is relatively regular, it can be stored in database, form specific region Attribute data storehouse in case reuse.When user builds the three dimension strata model in modeling region, the brill in region can extract The related information of hole data, cross-sectional data and other altitude datas, such as contour, elevational point, and carry out coupling merger processing, Them is turned into the valid data during three-dimensional geological modeling, be that the structure of model establishes data basis.The modeling method In practical application, for specific modeling region, numerous drilling is might have, the information that these drillings can be provided Hierarchical information of position (geographical coordinate) including each drilling, the type of drilling and stratum etc..In view of some information Distribution of boreholes is closeer, and used drilling hole amount is huge when being modeled in the range of a wide range of or even whole research area, can not only reduce Modeling efficiency, is also unfavorable for the analysis and research to model, at this moment it is contemplated that drilling is classified according to certain net degree, when entering During row modeling according to the size (can one standard of predefined) of modeling scope calculate used in drilling rank, Ran Houzai Extracting the borehole data of appropriate level is used to model.
Step b), use the borehole data in the multi-source data that step a) extracts with building the region of covering whole modeling region Sequence table layer by layer.One notable feature on stratum be it into " layer " property, belong to the stratum of same " layer " have it is unanimous on the whole Sedimentary Age and mechanics index of physics, same type of material is can be regarded as to a certain extent.The layering of borehole data Information is the description of the contact surface to neighbouring stratum, can disclose vertical distribution situation of the stratum at bore position.Time Drillings all in modeling region are gone through, is picked out and is disclosed a most drilling of rock stratum information and make the formation information of this drilling For initial stratigraphic sequence table, then this sequence table is compared one by one with residue drilling, if sequence is inconsistent, sequence is updated Table, if unanimously, skipping Present Borehole, continues more next drilling, so repeatedly, and it is complete that modeling region is covered in generation one The regional stratum sequence table on portion stratum, in case follow-up modeling is used.Carrying out the rule of stratum numbering is:, to old, successively passed from newly Increase.I.e. newest stratum numbering is 1, is then gradually incremented by according to stratum age.
Step c), borehole formation aspect is numbered.Each stratum and region in region in each drilling will be modeled Stratigraphic sequence table is contrasted, and is determined the sequence number of each formation beds in each drilling, is ignored non-existent stratum in the drilling.Compile Number rule is:From top to bottom, since 0.That is the serial number 0 of drilling top formation beds (ground surface), with each in drilling Stratum is corresponding in regional stratum sequence table to number to specify the numbering of the formation beds of the stratum bottom surface in drilling.Separately Outside, do not have influential, insignificant substratum on final modeling result, merger processing can be carried out in borehole formation aspect numbering, Do not considered during actual modeling.
Step d), the aspect template on each stratum of generation.The generation of each formation beds template, refers to in the formation beds On the basis of the aperture coordinate of all drillings, with reference to modeling regional boundary condition, one generated using the triangulation of standard The individual triangulation network.The formation beds template define not only the external boundary of three dimension strata model to be built, additionally it is possible to expression modeling The topological relation of each formation beds of region.It is considered as being to determine one " template " of modeling regional stratum topological relation, Can from top to bottom it put off along drilling depth to whole stratum in modeling region.It can so ensure that each formation beds has Topological relation determine, unanimous between the higher and lower levels, can greatly simplify the complexity of subsequent treatment, strengthen the robustness of algorithm.
Step e), using multi-source data row interpolation is entered to formation beds elevation.The bed boundary of TIN formation Although can truly reflect display situation, due to the inhomogeneity of data, the curved surface of formation often very irregular need to be inserted Value is smooth.Kriging regression method is used in the embodiment of the present invention, using the multi-source data of extracted coupling to the stratum of generation Aspect carries out smooth.Extract the elevation information at each formation beds control point respectively, including data in bore database and cut open Control point data in the figure of face, using these point interpolations ask various regions layer by layer on face die plate each unknown point height value;If ground The point on face die plate is consistent with the two-dimensional plane coordinate drilled layer by layer, then the elevation of the point and the stratigraphic controls point disclosed in drilling Elevation is consistent, it is not necessary to interpolation.The main feature that Kriging regression is different from other spatial interpolation methods is, to the sky of variable Between correlation analyzed and utilized, can more objectively reflect geological phenomenon, the simple and direct practicality of algorithm, with certain extrapolation energy Power, application effect is good.
Step f), the intersecting processing of progress formation beds, then adjust stratum elevation.When carrying out interpolation fitting to stratum, The data on correspondence stratum are only considered, interpolation and the fitting on each stratum are independent progress, thus do not account for adjacent earth formations Crossover phenomenon between face.It so may result in form the cross one another situation of multilayer digital elevation, this does not obviously square with the fact, Accordingly, it would be desirable to the intersecting processing of formation beds be carried out, so that the local height value adjustment of the understratum for follow-up intersecting stratum Lay the foundation.Stratum template after the intersecting processing of formation beds, it is possible that the point that should be located on understratum Elevation, but higher than the stratum above it, this needs to adjust stratum elevation, pulls it back on the elevation equal with its last layer. This process is completed by comparing the corresponding point of each formation beds.For the specified point in specific formation beds TriPnti, its height value is Zi, the corresponding points TriPnt in a formation beds thereon can be retrievedi-1Height value Zi-1If, ZiMore than Zi-1, it is necessary to by ZiAgain it is entered as Zi-1, so just can guarantee that up and down the uniformity of surface layer order relation layer by layer.
Step g), structure three-dimensional formation physical model.Generate after each formation beds triangulation network, it is necessary to will be neighbouring The triangulation network of formation beds unites by a seam on vertical, you can constitute complete three-dimensional formation physical model.Only need to top layer or A triangle in bottom formation beds is all triangles on starting point, each stratum of circular treatment and each formation beds Shape can be completed.
In the embodiment of the present invention, the extracted data model with after coupling of multi-source data mainly has two kinds in step a):Ground Particle key element and geology line feature.Drilling and stratum isopleth data form ground particle feature model after extracting;Profile, geology Stage casing figure and geological structure diagram data can generate ground particle feature model and geology line feature model after extracting.Each class data are all The plug-in unit extracted by a data, which is realized, to be extracted, and data are generated corresponding point key element and line feature model by all plug-in units, These key elements are subjected to coupling processing again afterwards.Fig. 2 is refer to, the specific method for extracting multi-source data and being coupled is:
Step s1), the extraction of the main multi-source data such as drilling.For borehole data, due to drill purpose and it is affiliated specially The difference of industry causes the form of borehole data to have differences, but drill hole information has relative normalization again, it is therefore desirable to set The reasonable efficient bore database of meter one, is arranged and is standardized to original borehole data, borehole data is realized with this Integrated management, it is ensured that the validity and completeness of original drill hole information.Cross-sectional data is produced by two ways:One kind is user By borehole data hand drawn profile, there is the possibility of mistake than larger as modelling data source in this data;It is another It is that the knowledge such as expert's interpretation and Engineering borderline tracking is combined together using program to plant, and automatically generates the main body frame of profile, Connection and the editor for carrying out hatching on this basis by professional again.Obtaining terrestrial reference isopleth data typically has two kinds of sides Method:One kind is by geology personnel's manual drawing;Another is to enter row interpolation tracking by computer to form.
Step s2), the generation of three-dimensional geological key element.Will drilling point data, section diagram data, isopleth data and plane earth Matter diagram data etc. is converted into three-dimensional geological key element:Drill key element, section key element, geological plane maps key element etc..
Wherein, the process of the generation of drilling key element actually drilling modeling, the drilling includes straight hole data and oblique Hole data.The embodiment of the present invention is by taking inclined hole as an example, and straight hole is considered as a kind of its special case.From earth's surface to underground, inclined hole needs note Record the buried depth and angle (zenith angle and azimuth) of each point.If hell coordinate is P0(x0, y0, z0), each point of underground Depth be DEPi, and zenith angle and azimuth are respectively AiAnd Bi, then each point of underground Pi(xi, yi, zi) coordinate be:
xi=x0-DEPi*tg(Ai)*cos(Bi)
yi=y0-DEPi*tg(Ai)*sin(Bi)
zi=z0-DEPi
According to P0、P1、…、Pi... coordinate can set up the pipeline model of drilling.
The geologic datas such as the earth's surface isopleth data, planogram data, are present in the form of two-dimensional visualization In map, it need to be changed to three-dimensional coordinate.Because the line feature of isopleth data has Height attribute field, its two-dimensional line holds very much Easily it is converted into three-dimensional line.For plane geologic data, it is necessary to which each key element on two-dimensional structure (point) line is carried out into linear translation, The three-dimensional coordinate matched is obtained, then height value is adjusted in the three-dimensional model.
For two-dimensional cross section, profile is matched with three-dimensional drilling, and then the three-dimensional coordinate put on reference section line, Comparatively it is more difficult.In embodiments of the present invention, profile is positioned using survey line, according to position of the hatching in profile And the actual coordinate value positioning the entire profile position in space in space, if known to two in profile of hatching Coordinate points are P0(mx0, my0) and P1(mx1, my1), two coordinate points Ks of the corresponding hatching in section space0(fx0, fy0, fz0) and K1(fx1, fy1, fz1).Then the corresponding three-dimensional in arbitrfary point (x, y) in two dimensional cross-section can be calculated according to similar triangles theorem Coordinate points P (X, Y, Z):
Map represents map reference, is abbreviated as m, and fact represents actual coordinate, writes a Chinese character in simplified form f.
Therefore, in above-mentioned formula:
mx0、my0Abscissa, the ordinate in geographical base map two dimensional cross-section on certain point diagram are represented respectively;
mx1、my1Abscissa, the ordinate in geographical base map two dimensional cross-section on another point diagram are represented respectively;
fx0、fy0、fz0The actual abscissa of D profile space point, ordinate, elevation are represented respectively;
fx1、fy1、fz1The actual abscissa of another point in D profile space, ordinate, elevation are represented respectively.
According to above-mentioned coordinate transformation formula, two dimensional cross-section line is converted into D profile line, then hang up it is existing up and down Layer attribute, forms section line feature;On the basis of section line feature, the ground layer line to closing carries out triangulation, forms son Face, hangs up attribute formation cross-sectional area key element.
Step s3), the coupling processing of multi-source data.Data coupling is carried out to three-dimensional geological key element, three new dimensions are formed According to key element:Ground particle key element, geology line feature.Carry out the stratum containing standard complex layered geology three-dimensional modeling when, it is necessary to according to Attribute conditions and steric requirements search ground particle and geology line feature, are then modeled.
Drilling, stratum top plate isogram and profile are to be completed by different professionals in different times, therefore, During the multi-source data coupling processing is carried out, there can be certain contradiction.When there is contradiction, it is necessary to enter to data Row consistency adjustment.Because borehole data is relatively believable data, during the principle of stratum inconsistency adjustment, to drill It is basic control framework, the other data sources of adjustment with cross-sectional data.
It refer in Fig. 3, the embodiment of the present invention, when carrying out intersecting processing to formation beds, each formation beds is By many triangle sets into determining whether there is intersecting between two formation beds models, it is necessary to carry out a large amount of triangle pairs Intersecting detection, therefore, formation beds cap is relatively time consuming.The method of the intersecting processing of formation beds is in step f): Using the collision detection algorithm based on AABB-OBB borders, collision detection is carried out to the formation beds triangulation network, comprised the following steps that:
Step 1), in units of single formation beds build formation beds AABB detection storehouse detected, it is assumed that model Include N number of stratum in region, then need to build the AABB detections storehouse of N number of formation beds.
Step 2), only projections of two AABB in three reference axis just to can be regarded as two AABB when having overlapping intersecting, Detect that storehouse and other AABB detect that the AABB between storehouse, to being compared, finds out intersecting AABB pairs, n to n-th of AABB accordingly Initial value be 1, if not intersecting between two AABB pairs of formation beds, constitute stratal surface triangle be also impossible to phase Hand over.
Step 3), blow intersecting AABB pairs, set up in units of triangle OBB detection storehouse carry out collision detection, find out The triangle pair intersected in corresponding OBB.
Step 4), more accurate positioning intersection algorithm is carried out to intersecting triangle, judge whether it really intersecting, and ask Go out intersection point.
Step 5), the triangle that is detected in the aspect of understratum is deleted, using step 4) in the intersection point that calculates as new Control point, triangulation is re-started to understratum aspect.
Step 6), judge whether to have traveled through all formation beds, if not having, return to step 2) restart circulation, if Compare, then intersected processing and complete.
Above content is to combine the further description that specific embodiment is done to the present invention, it is impossible to assert this hair Bright specific implementation is confined to these explanations.For the those of ordinary skill of the technical field belonging to the present invention, not On the premise of departing from present inventive concept, some simple deduction or replace can also be made, are regarded as belonging to the protection of the present invention Scope.

Claims (6)

1. the stratified geological objects modeling method of the multi-source data coupling on the stratum containing standard, it is characterised in that:It comprises the following steps:
A) selection modeling region, extracts multi-source data and is coupled;
B) borehole data in the multi-source data of step a) extractions is used to build the regional stratum sequence table for covering whole modeling region;
C) each drilling in the modeling region is compareed with the regional stratum sequence table respectively, it is determined that each drilling In contained all stratum aspect sequence number;
D) on the basis of all drilling orifice coordinates included in each stratum, with reference to modeling regional boundary condition, cutd open using triangle The algorithm generation triangulation network is divided to form the aspect on each stratum;
E) row interpolation is entered to the aspect elevation on each stratum of generation in step d) with the multi-source data that coupling is extracted through step a), with The aspect on smooth each stratum;
F) formation beds after step e) processing are subjected to intersecting processing, and stratum elevation is adjusted according to the sequence on stratum;
G) triangulation network of neighbouring formation beds is sutured on vertical, constitutes complete three-dimensional geological physical model.
2. the stratified geological objects modeling method of the multi-source data coupling on the stratum as claimed in claim 1 containing standard, its feature exists In:The specific method that multi-source data is extracted in step a) and is coupled is:S1 multi-source data) is extracted;S2) by step s1) in The multi-source data of extraction is converted into three-dimensional geological key element;S3) to step s2) in three-dimensional geological key element couple, formed ground Particle key element and geology line feature.
3. the stratified geological objects modeling method of the multi-source data coupling on the stratum as claimed in claim 1 containing standard, its feature exists In:The specific method of the structure regional stratum sequence table is in step b):Travel through the brills all in the modeling region Hole, picks out and discloses a most drilling of rock stratum information, and using its formation information as initial stratigraphic sequence table, then will just Beginning stratigraphic sequence table is compared one by one with residue drilling, if both sequences are inconsistent, updates sequence table, if both sequences are consistent, Present Borehole is then skipped, continues more next drilling, so repeatedly, the region on the whole stratum in modeling region is covered in generation one Stratigraphic sequence table.
4. the stratified geological objects modeling method of the multi-source data coupling on the stratum as claimed in claim 1 containing standard, its feature exists In:The specific method of the aspect sequence number on all stratum contained in each drilling of determination is in step c):To with drilling top Face is numbered layer by layer, then corresponding in regional stratum sequence table from top to bottom to number to determine each stratum in drilling Bottom surface formation beds numbering, and ignore the numbering in the drilling of present collation corresponding to non-existent stratum.
5. the stratified geological objects modeling method of the multi-source data coupling on the stratum as claimed in claim 1 containing standard, its feature exists In:Row interpolation is entered using Kriging regression method in step e), its specific method is:Each formation beds control point is extracted respectively Elevation information, the height value of each unknown point in formation beds is obtained with the control point interpolation;If point in formation beds with The coordinate of drilling is consistent, then does not need interpolation.
6. the stratified geological objects modeling method of the multi-source data coupling on the stratum containing standard as described in any one of claim 1 to 5, It is characterized in that:The specific method of adjustment stratum elevation is in step f):Certain point TriPnt in some formation bedsi, institute State point TriPntiHeight value be Zi, point TriPnt can be retrievediWith the corresponding points TriPnt in a upper formation bedsi-1, it is described Point TriPnti-1Height value be Zi-1If, ZiMore than Zi-1, then by ZiAgain it is entered as Zi-1
CN201710310068.3A 2017-05-02 2017-05-02 The stratified geological objects modeling method of the multi-source data coupling on the stratum containing standard Pending CN107180452A (en)

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Cited By (8)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN107944086A (en) * 2017-10-27 2018-04-20 江苏普旭软件信息技术有限公司 A kind of fast modeling method based on borehole data
CN109859312A (en) * 2019-02-01 2019-06-07 上海勘察设计研究院(集团)有限公司 A kind of fining three-dimensional geological model modeling method based on BIM technology
CN111784832A (en) * 2020-06-22 2020-10-16 长江大学 Stratum dynamic correction method of geological model
CN112084548A (en) * 2019-06-14 2020-12-15 中南大学 2.5D visual modeling method and system for slope stability analysis
CN112381937A (en) * 2020-11-03 2021-02-19 广东省地质调查院 Multi-source geological data coupling modeling method based on drilling and complex geological profile
CN113326606A (en) * 2021-05-08 2021-08-31 北京金阳普泰石油技术股份有限公司 Control line-based stratigraphic structure fluctuation representation processing method and system
CN116612248A (en) * 2023-05-08 2023-08-18 北京龙软科技股份有限公司 Stratum space expansion and modeling method based on mark layer and control point
CN117132723A (en) * 2023-08-23 2023-11-28 北京龙软科技股份有限公司 Method and device for extracting profile data for constructing coal seam geological model

Citations (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN102254349A (en) * 2011-06-30 2011-11-23 华东师范大学 Method for constructing three-dimensional physical model of sedimentary stratum system by using drilling data
CN103514631A (en) * 2013-10-21 2014-01-15 重庆市勘测院 Gridding type parallel construction method for three-dimensional geological model based on massive borehole data
US20140081613A1 (en) * 2011-11-01 2014-03-20 Austin Geomodeling, Inc. Method, system and computer readable medium for scenario mangement of dynamic, three-dimensional geological interpretation and modeling
CN105205864A (en) * 2015-08-26 2015-12-30 中国电建集团北京勘测设计研究院有限公司 Multi-source-data-based automatic modeling method and system of three-dimension model of geological structural surface

Patent Citations (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN102254349A (en) * 2011-06-30 2011-11-23 华东师范大学 Method for constructing three-dimensional physical model of sedimentary stratum system by using drilling data
US20140081613A1 (en) * 2011-11-01 2014-03-20 Austin Geomodeling, Inc. Method, system and computer readable medium for scenario mangement of dynamic, three-dimensional geological interpretation and modeling
CN103514631A (en) * 2013-10-21 2014-01-15 重庆市勘测院 Gridding type parallel construction method for three-dimensional geological model based on massive borehole data
CN105205864A (en) * 2015-08-26 2015-12-30 中国电建集团北京勘测设计研究院有限公司 Multi-source-data-based automatic modeling method and system of three-dimension model of geological structural surface

Non-Patent Citations (2)

* Cited by examiner, † Cited by third party
Title
吴志春等: "三维地质建模中的多源数据融合技术与方法", 《吉林大学学报》 *
朱良峰等: "基于钻孔数据的三维地层模型的构建", 《地理与地理信息科学》 *

Cited By (14)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN107944086B (en) * 2017-10-27 2021-02-05 江苏普旭软件信息技术有限公司 Rapid modeling method based on drilling data
CN107944086A (en) * 2017-10-27 2018-04-20 江苏普旭软件信息技术有限公司 A kind of fast modeling method based on borehole data
CN109859312A (en) * 2019-02-01 2019-06-07 上海勘察设计研究院(集团)有限公司 A kind of fining three-dimensional geological model modeling method based on BIM technology
CN112084548A (en) * 2019-06-14 2020-12-15 中南大学 2.5D visual modeling method and system for slope stability analysis
CN112084548B (en) * 2019-06-14 2022-06-07 中南大学 2.5D visual modeling method and system for slope stability analysis
CN111784832B (en) * 2020-06-22 2024-01-09 长江大学 Stratum dynamic correction method of geological model
CN111784832A (en) * 2020-06-22 2020-10-16 长江大学 Stratum dynamic correction method of geological model
CN112381937A (en) * 2020-11-03 2021-02-19 广东省地质调查院 Multi-source geological data coupling modeling method based on drilling and complex geological profile
CN112381937B (en) * 2020-11-03 2024-03-12 广东省地质调查院 Multi-source geological data coupling modeling method based on drilling and complex geological profile
CN113326606A (en) * 2021-05-08 2021-08-31 北京金阳普泰石油技术股份有限公司 Control line-based stratigraphic structure fluctuation representation processing method and system
CN113326606B (en) * 2021-05-08 2023-08-15 北京金阳普泰石油技术股份有限公司 Control line-based stratum structure fluctuation characterization processing method and system
CN116612248A (en) * 2023-05-08 2023-08-18 北京龙软科技股份有限公司 Stratum space expansion and modeling method based on mark layer and control point
CN116612248B (en) * 2023-05-08 2024-02-06 北京龙软科技股份有限公司 Stratum space expansion and modeling method based on mark layer and control point
CN117132723A (en) * 2023-08-23 2023-11-28 北京龙软科技股份有限公司 Method and device for extracting profile data for constructing coal seam geological model

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Application publication date: 20170919