CN111044600A - Elemental geochemical method for identifying ore body center of sodium-assisted uranium deposit - Google Patents
Elemental geochemical method for identifying ore body center of sodium-assisted uranium deposit Download PDFInfo
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- CN111044600A CN111044600A CN201911401374.3A CN201911401374A CN111044600A CN 111044600 A CN111044600 A CN 111044600A CN 201911401374 A CN201911401374 A CN 201911401374A CN 111044600 A CN111044600 A CN 111044600A
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Abstract
The invention belongs to the technical field of geological exploration, and particularly relates to an element geochemistry method for identifying the center of a sodium-assisted uranium deposit ore body. The invention comprises the following steps: firstly, collecting various rock ore samples in a sodium-assisted uranium deposit by a system; analyzing the trace element content of the collected sample; and thirdly, analyzing the spatial variation characteristics and rules of the trace element content in the sodium-substituted uranium deposit, and dividing characteristic element combinations in different mineralization zones so as to predict and judge the center of the sodium-substituted uranium deposit ore body. The method can simply, quickly and effectively identify the center of the sodium alternate uranium deposit ore body, and provides technical support for the exploration and the ore finding of the sodium alternate uranium deposit and the prediction of the ore formation.
Description
Technical Field
The invention belongs to the technical field of geological exploration, and particularly relates to an element geochemistry method for identifying the center of a sodium-assisted uranium deposit ore body.
Background
The sodium-handed uranium deposit is a very important type of hydrothermal uranium deposit produced in ukraine, australia, canada, brazil, karilong, magas, usa, caragana, czech, etc.
Although the average grade of uranium of the sodium cross-substitution type uranium deposit is much lower than that of other types of uranium deposits, the content of uranium resources can be comparable with that of globally known non-integrated surface type uranium deposits, a large-scale uranium mineralization zone is formed, and the uranium mineralization zone has a good prospect of prospecting.
The sodium-mixed uranium deposit is relatively developed in a uranium mineralization zone from Qilian mountain to Longshou mountain in China, such as splendid achnatherum, a new water well, a Bandu mouth and the like. However, the ore deposit discovered in China at present is small in scale and complex in ore body form, so that the deep mineralization potential of the existing sodium alternate uranium ore deposit is difficult to accurately determine, and the exploration result is difficult to break through.
Due to the influence of the multiple stages and sources of the mineralization process and the distribution and migration rules of elements in the geologic body, geochemical elements in the mineralization area show the characteristics of symbiotic combination halo in space.
Therefore, research on an element geochemical method for identifying the ore body center of the sodium-substitution uranium deposit is developed so as to rapidly and objectively evaluate the deep mineralization potential of the existing sodium-substitution uranium deposit, thereby achieving the purpose of effectively and economically solving the geological problem and obtaining a good ore finding effect.
Disclosure of Invention
The technical problems solved by the invention are as follows:
the invention aims to provide an element geochemical method for identifying the ore body center of a sodium-substitution type uranium deposit, which can accelerate the ore finding speed, improve the ore finding hit rate and reduce the exploration cost.
The technical scheme adopted by the invention is as follows:
an element geochemical method for identifying a sodium-assisted uranium deposit ore body center comprises the following steps:
firstly, collecting various rock ore samples in a sodium-assisted uranium deposit by a system;
analyzing the trace element content of the collected sample;
and thirdly, analyzing the spatial variation characteristics and rules of the trace element content in the sodium-substituted uranium deposit, and dividing characteristic element combinations in different mineralization zones so as to predict and judge the center of the sodium-substituted uranium deposit ore body.
In the first step, according to the requirements of geological exploration specifications of the uranium ores, rock ore samples of the periphery of an ore body, the upper part of the ore body, the middle part of the ore body, the lower part of the ore body and a root phase in the sodium cross-substitution type uranium ore deposit are collected systematically.
And in the second step, according to the requirements of rock geochemistry analysis specifications, analyzing the contents of the trace ELEMENTs in the processed rock ore sample by using an ELEMENT plasma physical analyzer.
And in the third step, the contents of the trace elements in various rock ore samples in the obtained sodium-substituted uranium deposit are counted and analyzed through software.
The software comprises Excel, SAS, SPSS and S-plus.
By analyzing the change rule of the content of various trace elements on the space, the characteristic element combination halos in different mineralization zones are counted, so that the halos are used for predicting and distinguishing the center of the sodium-substitution uranium deposit ore body.
The analysis result is as follows:
within seventy-eighty meters above the sodium-substituted uranium ore body, obvious U, Th, Y, V and Pb compound halos exist, the scale of the U, Th and V halos is similar to or larger than that of the ore body, the scale of Y, Pb is small, and the distribution is sporadic; the Y, Pb part where the ore body is located is increased in scale, the strength is increased, the V-shaped halo is increased along with the depth, the strength is reduced, the scale is reduced, and Co-shaped halo appears; the Y, V, Pb halos became smaller and the Co halos became larger in size at the root and below of the ore than the U halos.
The invention has the beneficial effects that:
(1) the method can simply, quickly and effectively identify the center of the sodium alternate uranium deposit ore body, and provides technical support for the exploration and the ore formation prediction of the sodium alternate uranium deposit;
(2) the method has the advantages of wide coverage, strong applicability and high accuracy. The method has an important guiding function on deep exploration of sodium alternate uranium ores in China, and has a wide popularization and application prospect.
Detailed Description
The present invention will be described in further detail with reference to the following examples:
the invention provides an elemental geochemical method for identifying the center of a sodium-assisted uranium deposit ore body, which comprises the following steps:
firstly, collecting various rock ore samples in a sodium-assisted uranium deposit by a system;
according to the requirements of uranium ore geological exploration specifications, rock ore samples of the periphery of an ore body, the upper part of the ore body, the middle part of the ore body, the lower part of the ore body and an ore root phase in a certain sodium alternate type uranium ore deposit in China are collected systematically.
Analyzing the trace element content of the collected sample;
according to the requirements of rock geochemistry analysis specifications, pre-treatment such as sample crushing, weighing and the like is carried out on collected samples, and the treated rock ore samples are subjected to trace ELEMENT content analysis by using an ELEMENT plasma physical analyzer.
Including 44 items of Th, U, Sc, V, Pb, Co, Y, Cu, Mo, etc.
And thirdly, analyzing the spatial variation characteristics and rules of the trace element content in the sodium-substituted uranium deposit, and dividing characteristic element combinations in different mineralization zones so as to predict and judge the center of the sodium-substituted uranium deposit ore body.
And (3) counting and analyzing the trace element content of various rock ore samples in the obtained sodium-substituted uranium deposit through software such as Excel, SAS, SPSS, S-plus and the like, analyzing the change rule of the trace element content on the space, and counting the combination halos of the characteristic elements in different mineralization zones.
Statistical analysis shows that the obvious U, Th, Y, V and Pb composite halos are found in the range of seventy-eighty meters above the sodium-substituted uranium ore body, the scale of the U, Th and V halos is similar to or larger than that of the ore body, the scale of Y, Pb is small, and the distribution is sporadic; the Y, Pb part where the ore body is located is increased in scale, the strength is increased, the V-shaped halo is increased along with the depth, the strength is reduced, the scale is reduced, and Co-shaped halo appears; the Y, V, Pb halos became smaller and the Co halos became larger in size at the root and below of the ore than the U halos.
The present invention has been described in detail with reference to the embodiments, but the present invention is not limited to the embodiments, and various changes can be made without departing from the gist of the present invention within the knowledge of those skilled in the art. The prior art can be adopted in the content which is not described in detail in the invention.
Claims (7)
1. An element geochemical method for identifying the ore body center of a sodium-assisted uranium deposit is characterized by comprising the following steps: the method comprises the following steps:
firstly, collecting various rock ore samples in a sodium-assisted uranium deposit by a system;
analyzing the trace element content of the collected sample;
and thirdly, analyzing the spatial variation characteristics and rules of the trace element content in the sodium-substituted uranium deposit, and dividing characteristic element combinations in different mineralization zones so as to predict and judge the center of the sodium-substituted uranium deposit ore body.
2. The elemental geochemistry method for identifying the ore body center of sodium-substituted uranium deposit according to claim 1, wherein: in the first step, according to the requirements of geological exploration specifications of the uranium ores, rock ore samples of the periphery of an ore body, the upper part of the ore body, the middle part of the ore body, the lower part of the ore body and a root phase in the sodium cross-substitution type uranium ore deposit are collected systematically.
3. The elemental geochemistry method for identifying the ore body center of sodium-substituted uranium deposit according to claim 1, wherein: and in the second step, according to the requirements of rock geochemistry analysis specifications, analyzing the contents of the trace ELEMENTs in the processed rock ore sample by using an ELEMENT plasma physical analyzer.
4. The elemental geochemistry method for identifying the ore body center of sodium-substituted uranium deposit according to claim 1, wherein: and in the third step, the contents of the trace elements in various rock ore samples in the obtained sodium-substituted uranium deposit are counted and analyzed through software.
5. The elemental geochemistry method for identifying the ore body center of sodium-substituted uranium deposit according to claim 4, wherein: the software comprises Excel, SAS, SPSS and S-plus.
6. The elemental geochemistry method for identifying the ore body center of sodium-substituted uranium deposit according to claim 4, wherein: by analyzing the change rule of the content of various trace elements on the space, the characteristic element combination halos in different mineralization zones are counted, so that the halos are used for predicting and distinguishing the center of the sodium-substitution uranium deposit ore body.
7. The elemental geochemistry method for identifying the ore body center of sodium-substituted uranium deposit according to claim 6, wherein: the analysis result is as follows:
within seventy-eighty meters above the sodium-substituted uranium ore body, obvious U, Th, Y, V and Pb compound halos exist, the scale of the U, Th and V halos is similar to or larger than that of the ore body, the scale of Y, Pb is small, and the distribution is sporadic; the Y, Pb part where the ore body is located is increased in scale, the strength is increased, the V-shaped halo is increased along with the depth, the strength is reduced, the scale is reduced, and Co-shaped halo appears; the Y, V, Pb halos became smaller and the Co halos became larger in size at the root and below of the ore than the U halos.
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Citations (4)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| CN107632036A (en) * | 2017-08-04 | 2018-01-26 | 核工业北京地质研究院 | A kind of lithogeochemical method for identifying sodic-metasomatism type uranium deposit bed |
| CN108181669A (en) * | 2017-12-25 | 2018-06-19 | 核工业北京地质研究院 | A kind of hot spot active region U metallogeny recognition positioning method |
| CN108446530A (en) * | 2018-03-08 | 2018-08-24 | 中国地质科学院地质力学研究所 | A kind of geochemical elements anisotropy space Quantitative Analysis Method |
| CN109188556A (en) * | 2018-08-28 | 2019-01-11 | 国家海洋局第二海洋研究所 | A kind of Seafloor Sulfide method of prospecting based on terrain analysis |
-
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Patent Citations (4)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| CN107632036A (en) * | 2017-08-04 | 2018-01-26 | 核工业北京地质研究院 | A kind of lithogeochemical method for identifying sodic-metasomatism type uranium deposit bed |
| CN108181669A (en) * | 2017-12-25 | 2018-06-19 | 核工业北京地质研究院 | A kind of hot spot active region U metallogeny recognition positioning method |
| CN108446530A (en) * | 2018-03-08 | 2018-08-24 | 中国地质科学院地质力学研究所 | A kind of geochemical elements anisotropy space Quantitative Analysis Method |
| CN109188556A (en) * | 2018-08-28 | 2019-01-11 | 国家海洋局第二海洋研究所 | A kind of Seafloor Sulfide method of prospecting based on terrain analysis |
Non-Patent Citations (4)
| Title |
|---|
| 何光辉 等: "庐山沙溪斑岩型铜金矿床绿泥石的地球化学特征及找矿指示", 《矿床地质》 * |
| 地质矿产部地质辞典办公室 编: "《地质大辞典（五） 地质普查勘探技术方法分册 下册》", 30 June 2005, 地质出版社 * |
| 宿晓静 等: "黑龙江金厂金矿床J0号矿体地球化学特征及其找矿", 《世界地质》 * |
| 贾三石 等: "辽西排山楼金矿床微量元素地球化学特征及深部找矿预测研究", 《地球化学》 * |
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Application publication date: 20200421 |