CN109614741A - The strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity - Google Patents

The strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity Download PDF

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CN109614741A
CN109614741A CN201811593298.6A CN201811593298A CN109614741A CN 109614741 A CN109614741 A CN 109614741A CN 201811593298 A CN201811593298 A CN 201811593298A CN 109614741 A CN109614741 A CN 109614741A
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许强
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Beijing Research Institute of Uranium Geology
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Beijing Research Institute of Uranium Geology
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Abstract

The invention belongs to uranium exploration technical fields, and in particular to a kind of strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity.The present invention prepares regional geologic map the following steps are included: step 1;Step 2 determines destination layer;Step 3, establishment deposition phasor, irises out favorable sedimentary facies belt range;Step 4 irises out construction and is lifted relatively weak range;Step 5 irises out earth's surface radioactive anomaly range;Step 6 irises out uranium exception distribution of boreholes range;Step 7 irises out secondary oxidation zone range;Step 8 irises out radon anomalies range;Step 9 predicts prospective area.The present invention provides the factors such as sufficiently comprehensive sedimentary facies, tectonic activity, oxidized zone, drilling exception, earth's surface radioactive anomaly, Anomaly recognition exception, the strongly regional sandstone-type uranium deposit prospective area of integrated forecasting neotectonics activity.

Description

The strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity
Technical field
The invention belongs to uranium exploration technical fields, and in particular to a kind of strongly regional sandstone-type uranium deposit of neotectonics activity Predication of Prospective Areas method.
Background technique
Neotectonic movement tectonic activity is strong, uplift erosion is strong, destroys the sandstone uranium mineralization and oxidized zone of early formation, Great difficulty is caused in such regional sandstone Prospecting For Uranium.China's neotectonic movement coverage is extensive, on such ground Area's prediction sandstone Prospective area for uranium is badly in need of a kind of effective method, therefore establishes a kind of strongly regional sandstone of neotectonics activity Type Prospective area for uranium prediction technique is extremely necessary.
Summary of the invention
The technical problem to be solved by the present invention is to big for the strongly regional Prospecting Sandstone-type Uranium Deposits difficulty of neotectonics activity The problem of, a kind of strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity is provided, deposition can be sufficiently integrated The factors such as phase, tectonic activity, oxidized zone, earth's surface radioactive anomaly, Anomaly recognition exception, the strongly regional sand of prediction neotectonics activity Lithotype Prospective area for uranium.
The technical solution adopted in the present invention:
The strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity, includes the following steps:
Step 1 prepares regional geologic map: collecting the regional geologic map of area's Prospective area for uranium to be predicted, geologic map ratio Ruler is 1:25 ten thousand, 1:20 ten thousand, 1:5 Wan Junke;
Step 2 determines destination layer: investigating region geologic information to be predicted, carries out outcrop investigation, investigates drilling well Core gets colors containing carbon dust, folder seam, the group in coal seam to be destination layer in grey, sandstone;
Step 3, establishment deposition phasor, iris out favorable sedimentary facies belt range: area to be predicted carry out geological profile survey, Mineral product geology investigation is edited and recorded data according to profile survey, investigation result of appearing, drilling, it is heavy that area to be predicted is worked out as unit of group Product phasor, Division of Sedimentary Facies band, Mapgis vector quantization have the deposition phasor of projection coordinate's system;In the heavy of Mapgis vector quantization In product phasor, Sedimentary Model of Braided River Facies, braided river delta, meandering river facies, meandering stream delta phase are selected, is irised out with multiple spot broken line Close range, as favorable sedimentary facies belt range;
Step 4 irises out construction and is lifted relatively weak range: according to mineral product geology investigation result, irising out structure on geologic map It makes and is lifted relatively weak region;
Step 5 irises out earth's surface radioactive anomaly range: carrying out the area measurement of earth's surface gamma-ray spectrometry in area to be predicted, irises out Earth's surface radioactive anomaly point, abnormal belt and abnormal dizzy distribution;
Step 6 irises out uranium exception distribution of boreholes range: according to drilling radioactive logging curve, being gone out with organizing for unit selection With the drilling of radioactive anomaly in destination layer, and the drilling picked out to organize as cell projection at corresponding group of establishment It deposits in phasor;
Step 7 irises out secondary oxidation zone range: (1) by the group of destination layer that step 2 determine as unit of, screening drilling, Pick out the drilling of secondary oxidation;(2) as unit of the group for the destination layer that step 2 determines, the drilling of secondary oxidation is irised out Distribution;It is investigated according to mineral product geology, as unit of group;(3) it is irised out with multiple spot broken line secondary oxygen using mapgis software Change band range;
Step 8 irises out radon anomalies range: carrying out Anomaly recognition area measurement in area to be predicted, irises out radon anomalies Point, abnormal belt and abnormal dizzy distribution, using Mapgis software, iris out radon anomalies point, abnormal belt, abnormal dizzy distribution Range is projected on the geologic map of step 1 vector quantization;
Step 9 predicts prospective area: the construction that favorable sedimentary facies belt range that step 3 is irised out, step 4 are irised out is lifted Relatively weak range, step 5 iris out earth's surface radioactive anomaly range, step 6 is irised out abnormal distribution of boreholes range, step 7 The radon anomalies range that secondary oxidation zone range, the step 8 irised out are irised out all is projected in the areal geology of step 1 vector quantization On figure.
In the step 1, geologic map is Mapgis vector quantization electronics graph, and graph has projective parameter and coordinate.
In the step 3, profile survey scale bar requires to be not less than 1:10000, and scale bar is bigger, and compilation precision is higher; It is 1:50000 that mineral product geology, which investigates scale bar,;Sedimentary facies compilation scale bar requires to be not less than 1:250000, and the bigger volume of scale bar Figure precision is higher;Drilling hole amount is more, and compilation precision is higher.
In the step 4, construction is lifted relatively weak area judging foundation are as follows: the 1. relatively slow region of stratigraphic dip, 2. the end regions that pitch of fold, 3. develop the cross fracture region vertical with regional main construction line, cross fracture shows in landform For the river or valley for cutting through mountain range, landform is more gentle on region, and the covering of mostly the 4th system, which can be with 1 Separately as distinguishing rule, it a plurality of can also combine and be used as distinguishing rule.
In the step 4, construction lifting is irised out on the regional geologic map of step 1 vector quantization using Mapgis relatively Weak range irises out closed area with multiple spot broken line, and the region irised out can be arrived multiple for 1.
In the step 5, earth's surface gamma-ray spectrometry area measurement uses instrument requirements for four gamma spectrometers;Scale bar It is required that being not less than 1:500000, and scale bar is bigger, and it is higher to iris out earth's surface radioactive anomaly range accuracy;Measurement and abnormal point, Abnormal belt, extremely dizzy calculating execute specification " ground gamma-ray spectrometry specification (EJ/T363-1998) ".
In the step 7, it is grey, grey-green sandstone since secondary oxidation shows that secondary oxidation mark, which is primary, For yellow, red, aubergine, brown, visible grey agglomerate residual in sandstone is aoxidized;The secondary oxidation zone distribution that broken line is irised out Range is closed area, and secondary oxidation zone distribution can arrive multiple in single group for 1.
In the step 8, area measurement scale bar is not less than 1:10 ten thousand, and scale bar is bigger, and precision is higher;Measurement range Plane projection range will be located at step 3 in mark off in the following facies tract of sedimentary facies belt: pigtail river facies, braided river delta, Meandering stream, meandering stream delta phase;Radon gas area measurement method and abnormal point, abnormal belt, extremely dizzy calculating are referring to specification " radon And its daughter specifications of surveys (EJ/T 605-91) ".
In the step 9, the reliability of prospective area according to the range overlapping degree that above-mentioned steps three to step 8 are irised out come It determines, the higher region of overlapping degree, prospective area reliability is higher;Region except the sharp sedimentary facies belt range that step 3 is irised out It cannot function as prospective area;The region that the construction that step 4 is irised out is lifted except relatively weak range cannot function as prospective area.
Beneficial effects of the present invention: the present invention is big for the strongly regional sandstone Prospecting For Uranium difficulty of neotectonics activity, builds The method for having stood such a set of area prediction sandstone Prospective area for uranium prediction, can effectively save the time, improve efficiency.
Specific embodiment
Invention is further described in detail combined with specific embodiments below.
A kind of strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity provided by the invention, including it is following Step:
Step 1 prepares regional geologic map
With collecting the region that will predict strong regional (the area hereinafter referred to as to be predicted) Prospective area for uranium of neotectonics activity Matter figure, geology drawing scale are 1:25 ten thousand, 1:20 ten thousand, 1:5 Wan Junke.Step 1 requirement are as follows: geologic map is Mapgis vector quantization Electronics graph, graph have projective parameter and coordinate.
Step 2 determines destination layer
It investigates region geologic information to be predicted, carry out outcrop investigation, investigate drill core, get colors as ash In color, sandstone containing carbon dust, folder seam, the group in coal seam be destination layer.Destination layer can arrive several for 1.
Step 3, establishment deposition phasor, irises out favorable sedimentary facies belt range
Carry out geological profile survey, mineral product geology investigation in area to be predicted, according to profile survey, investigation result of appearing, bores Data is edited and recorded in hole, and deposition phasor in area's to be predicted, Division of Sedimentary Facies band are worked out as unit of group, and there is Mapgis vector quantization projection to sit The deposition phasor of mark system.
In the deposition phasor of Mapgis vector quantization, Sedimentary Model of Braided River Facies, braided river delta, meandering river facies, song are selected River delta facies is flowed, close range is irised out with multiple spot broken line, as favorable sedimentary facies belt range.
It is required in step 3 are as follows: (1) profile survey scale bar requires to be not less than 1:10000, the bigger compilation precision of scale bar It is higher;(2) mineral product geology investigation scale bar is 1:50000;(3) sedimentary facies compilation scale bar requires to be not less than 1:250000, and Scale bar is bigger, and compilation precision is higher;(4) drilling hole amount is more, and compilation precision is higher.
Step 4 irises out construction and is lifted relatively weak range
According to mineral product geology investigation result, construction is irised out on geologic map and is lifted relatively weak region.Construction lifting is opposite Weaker area judging foundation are as follows: the 1. relatively slow region of stratigraphic dip, 2. the end regions that pitch of fold, 3. develop and regionality The vertical cross fracture region of main construction line, cross fracture show as cutting through in landform the river or valley on mountain range, landform on region More gentle, the covering of mostly the 4th system, which can be with 1 separately as distinguishing rule, can also a plurality of combination conduct Distinguishing rule.
Step 4 requirement are as follows: iris out construction lifting on the regional geologic map of step 1 vector quantization using Mapgis relatively Weak range irises out closed area with multiple spot broken line, and the region irised out can be arrived multiple for 1.
Step 5 irises out earth's surface radioactive anomaly range
Carry out the area measurement of earth's surface gamma-ray spectrometry in area to be predicted, irises out earth's surface uranium abnormal point, abnormal belt and dizzy point of exception Cloth range.
Require in step 5: (1) area measurement of earth's surface gamma-ray spectrometry uses instrument requirements for four gamma spectrometers;(2): Scale bar requires to be not less than 1:500000, and scale bar is bigger, and it is higher to iris out earth's surface radioactive anomaly range accuracy;(3) it measures And abnormal point, abnormal belt, extremely dizzy calculating execute specification " ground gamma-ray spectrometry specification (EJ/T363-1998) ".
Step 6 irises out uranium exception distribution of boreholes range
According to drilling radioactive logging curve, to organize the drilling for going out in destination layer to have radioactive anomaly for unit selection, And the drilling picked out to organize as cell projection in corresponding group of establishment of deposition phasor.
Step 7 irises out secondary oxidation zone range
(1) as unit of the group for the destination layer that step 2 determines, the drilling of secondary oxidation is picked out in screening drilling;(2) As unit of the group of the destination layer determined by step 2, the distribution of boreholes range of secondary oxidation is irised out.It is investigated according to mineral product geology, As unit of group;(3) a secondary oxidation zone range is irised out with multiple spot broken line using mapgis software.
Require in step 7: (1) it is grey, grey-green sandstone due to secondary oxidation table that secondary oxidation mark, which is primary, Now it is yellow, red, aubergine, brown, aoxidizes visible grey agglomerate residual in sandstone;(2) the secondary oxidation that broken line is irised out Band distribution is closed area, and secondary oxidation zone distribution can arrive multiple in single group for 1.
Step 8 irises out radon anomalies range
Carry out Anomaly recognition area measurement in area to be predicted, iris out radon anomalies point, abnormal belt and abnormal dizzy distribution, Using Mapgis software, the radon anomalies point irised out, abnormal belt, abnormal dizzy distribution are projected in the ground of step 1 vector quantization On matter figure.
It is required in step 8 are as follows: (1) area measurement scale bar is not less than 1:10 ten thousand, and scale bar is bigger, and precision is higher;(2) The plane projection range of measurement range, which will be located in step 3, to be marked off in the following facies tract of sedimentary facies belt: pigtail river facies, braided stream Delta facies, meandering stream, meandering stream delta phase;(4) radon gas area measurement method and abnormal point, abnormal belt, extremely dizzy meter It calculates referring to specification " radon and its daughter specifications of surveys (EJ/T 605-91) ".
Step 9 predicts prospective area
The construction that favorable sedimentary facies belt range that step 3 is irised out, step 4 are irised out is lifted relatively weak range, step Five iris out earth's surface radioactive anomaly range, the secondary oxidation zone that the abnormal distribution of boreholes range that step 6 is irised out, step 7 are irised out The radon anomalies range that range, step 8 are irised out all is projected on the regional geologic map of step 1 vector quantization.
The requirement of step 9 are as follows: (1) reliability of prospective area is overlapped according to the range that above-mentioned steps three to step 8 are irised out Degree determines, the higher region of overlapping degree, and prospective area reliability is higher.(2) the sharp sedimentary facies belt range that step 3 is irised out Except region cannot function as prospective area.(3) region that the construction that step 4 is irised out is lifted except relatively weak range cannot be made For prospective area.

Claims (9)

1. the strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity, characterized by the following steps:
Step 1 prepares regional geologic map: collecting the regional geologic map of area's Prospective area for uranium to be predicted, geology drawing scale is 1:25 ten thousand, 1:20 ten thousand, 1:5 Wan Junke;
Step 2 determines destination layer: it investigates region geologic information to be predicted, carry out outcrop investigation, investigate drill core, It gets colors containing carbon dust, folder seam, the group in coal seam to be destination layer in grey, sandstone;
Step 3, establishment deposition phasor, irises out favorable sedimentary facies belt range: carrying out geological profile survey, mineral products in area to be predicted Geologic survey is edited and recorded data according to profile survey, investigation result of appearing, drilling, area's sedimentary facies to be predicted is worked out as unit of group Figure, Division of Sedimentary Facies band, Mapgis vector quantization have the deposition phasor of projection coordinate's system;In the sedimentary facies of Mapgis vector quantization In figure, Sedimentary Model of Braided River Facies, braided river delta, meandering river facies, meandering stream delta phase are selected, closing is irised out with multiple spot broken line Range, as favorable sedimentary facies belt range;
Step 4 irises out construction and is lifted relatively weak range: according to mineral product geology investigation result, construction lift is irised out on geologic map Rise relatively weak region;
Step 5 irises out earth's surface radioactive anomaly range: carrying out the area measurement of earth's surface gamma-ray spectrometry in area to be predicted, irises out earth's surface Radioactive anomaly point, abnormal belt and abnormal dizzy distribution;
Step 6 irises out uranium exception distribution of boreholes range: being that unit selection goes out target with group according to drilling radioactive logging curve There is the drilling of radioactive anomaly in layer, and the drilling picked out is organized corresponding group of the deposition for cell projection in establishment In phasor;
Step 7 irises out secondary oxidation zone range: (1) as unit of the group for the destination layer that step 2 determines, screening drilling is selected There is the drilling of secondary oxidation out;(2) as unit of the group for the destination layer that step 2 determines, the distribution of boreholes of secondary oxidation is irised out Range;It is investigated according to mineral product geology, as unit of group;(3) secondary oxidation zone is irised out with multiple spot broken line using mapgis software Range;
Step 8 irises out radon anomalies range: carrying out Anomaly recognition area measurement in area to be predicted, irises out radon anomalies point, different Often band and abnormal dizzy distribution, using Mapgis software, iris out radon anomalies point, abnormal belt, abnormal dizzy distribution It is projected on the geologic map of step 1 vector quantization;
Step 9 predicts prospective area: the construction that favorable sedimentary facies belt range that step 3 is irised out, step 4 are irised out is lifted opposite Weaker range, step 5 iris out earth's surface radioactive anomaly range, step 6 is irised out abnormal distribution of boreholes range, step 7 are irised out Secondary oxidation zone range, the radon anomalies range irised out of step 8 be all projected in the regional geologic map of step 1 vector quantization On.
2. the strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity according to claim 1, feature Be: in the step 1, geologic map is Mapgis vector quantization electronics graph, and graph has projective parameter and coordinate.
3. the strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity according to claim 2, feature Be: in the step 3, profile survey scale bar requires to be not less than 1:10000, and scale bar is bigger, and compilation precision is higher;Mineral products Geologic survey scale bar is 1:50000;Sedimentary facies makes picture scale bar requirement not less than 1:250000, and the bigger compilation of scale bar is smart It spends higher;Drilling hole amount is more, and compilation precision is higher.
4. the strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity according to claim 3, feature Be: in the step 4, construction is lifted relatively weak area judging foundation are as follows: the 1. relatively slow region of stratigraphic dip, 2. The end regions that pitch of fold, 3. develop the cross fracture region vertical with regional main construction line, and cross fracture is shown as in landform The river or valley on mountain range are cut through, landform is more gentle on region, and the covering of mostly the 4th system, which can be with 1 list It is solely used as distinguishing rule, a plurality of can also combine and be used as distinguishing rule.
5. the strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity according to claim 4, feature It is: in the step 4, it is relatively weak irises out construction lifting on the regional geologic map of step 1 vector quantization using Mapgis Range, closed area is irised out with multiple spot broken line, the region irised out can be for 1 to multiple.
6. the strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity according to claim 5, feature Be: in the step 5, earth's surface gamma-ray spectrometry area measurement uses instrument requirements for four gamma spectrometers;Scale bar requirement Not less than 1:500000, and scale bar is bigger, and it is higher to iris out earth's surface radioactive anomaly range accuracy;Measurement and abnormal point, exception Band, extremely dizzy calculating execute specification " ground gamma-ray spectrometry specification (EJ/T363-1998) ".
7. the strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity according to claim 6, feature Be: in the step 7, it is grey, grey-green sandstone since secondary oxidation shows as Huang that secondary oxidation mark, which is primary, Color, red, aubergine, brown aoxidize visible grey agglomerate residual in sandstone;The secondary oxidation zone distribution that broken line is irised out For closed area, secondary oxidation zone distribution can be for 1 to multiple in single group.
8. the strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity according to claim 7, feature Be: in the step 8, area measurement scale bar is not less than 1:10 ten thousand, and scale bar is bigger, and precision is higher;Measurement range is put down Face drop shadow spread, which will be located in step 3, to be marked off in the following facies tract of sedimentary facies belt: pigtail river facies, braided river delta, meander River, meandering stream delta phase;Radon gas area measurement method and abnormal point, abnormal belt, extremely dizzy calculating referring to specification " radon and its Daughter specifications of surveys (EJ/T 605-91) ".
9. the strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity according to claim 8, feature Be: in the step 9, the range that the reliability of prospective area is irised out according to above-mentioned steps three to step 8 overlaps degree to determine It is fixed, the higher region of degree is overlapped, prospective area reliability is higher;Region except the sharp sedimentary facies belt range that step 3 is irised out is not Prospective area can be used as;The region that the construction that step 4 is irised out is lifted except relatively weak range cannot function as prospective area.
CN201811593298.6A 2018-12-25 2018-12-25 The strongly regional sandstone-type uranium deposit Predication of Prospective Areas method of neotectonics activity Pending CN109614741A (en)

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CN113608278A (en) * 2021-07-26 2021-11-05 核工业北京地质研究院 Sandstone-type uranium ore positioning method in red heterolayer of sedimentary basin

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Application publication date: 20190412