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物探与化探  2022, Vol. 46 Issue (6): 1338-1348    DOI: 10.11720/wtyht.2022.1502
  地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
构造地球化学弱信息提取方法在黔西南卡林型金矿找矿中的应用
宋威方1,2(), 刘建中2,3,4(), 吴攀2,5, 李俊海4,6, 王泽鹏4,6, 杨成富4,6, 谭亲平7, 王大福6
1.湖北省地质局第六地质大队,湖北 孝感 432000
2.贵州大学 资源与环境工程学院,贵州 贵阳 550025
3.贵州省地质矿产勘查开发局,贵州 贵阳550004
4.自然资源部 基岩区矿产资源勘查工程技术创新中心,贵州 贵阳 550081
5.喀斯特地质资源与环境教育部重点实验室,贵州 贵阳 550025
6.贵州省地质矿产勘查开发局105地质大队,贵州 贵阳 550018
7.中国科学院地球化学研究所 矿床地球化学国家重点实验室,贵州 贵阳 550002
A successful application of the tectono-geochemistry weak information extraction method in the prospecting of Carlin-type gold deposits in southwestern Guizhou Province
SONG Wei-Fang1,2(), LIU Jian-Zhong2,3,4(), WU Pan2,5, LI Jun-Hai4,6, WANG Ze-Peng4,6, YANG Cheng-Fu4,6, TAN Qin-Ping7, WANG Da-Fu6
1. Six Geological Team of Hubei Geological Bureau,Xiaogan 432000,China
2. College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China
3. Bureau of Geology and Mineral Exploration and Development Guizhou Province, Guiyang 550004, China
4. Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources of the People's Republic of China, Guiyang 550018, China
5. Key Laboratory of Karst Geological Resources and Environment, Ministry of Education of the People's Republic of China, Guiyang 550025, China
6. No.105 Geological Team, Bureau of Geology and Mineral Exploration and Development Guizhou Province, Guiyang 550018, China
7. State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
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摘要 

本次研究介绍了构造地球化学测量理论的发展历程、研究现状及其应用效果,同时基于项目组在基岩区进行的找矿勘查实践,总结提炼最新研究成果和认识,提出了构造地球化学弱信息提取方法,并与传统的地球化学测量方法相对比,指出传统测量方法的局限性和构造地球化学弱信息提取方法的优越性。其次,系统归纳总结了构造地球化学弱信息提取方法的理论基础、工作条件、布点方法、采样原则、采样介质、异常解读和成图及其应用,重点突出构造地球化学弱信息提取方法中布点方法的合理性、采样点布置的代表性、采样介质的多样性、样品和元素异常信息的有效性(“有”和“无”),在此基础上构建构造地球化学弱信息提取方法指标体系。最后结合黔西南卡林型金矿分布区之灰家堡背斜东段找矿预测实践,认为构造地球化学弱信息提取方法较之传统的构造地球化学测量能够更加有效地提取深部成矿弱信息,在热液矿床隐伏矿找矿工作中具有较好的应用前景,可以推广到所有的基岩区热液矿床隐伏矿找矿预测工作中去。

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宋威方
刘建中
吴攀
李俊海
王泽鹏
杨成富
谭亲平
王大福
关键词 基岩区热液矿床找矿预测构造地球化学弱信息提取    
Abstract

This study introduced the development process, research status, and application effects of the tectono-geochemistry survey theory, and proposed the tectono-geochemistry weak information extraction method by summarizing the latest research results and understandings based on the prospecting practice in bedrock areas. Based on the contrastive analysis, this study pointed out the limitations of the conventional geochemical survey methods and the advantages of the tectono-geochemistry weak information extraction method, which was developed from the conventional tectono-geochemistry survey method. Moreover, this study systematically summarized the theoretical basis, operating conditions, deployment method, sampling principle, sampling media, anomaly interpretation, mapping, and application of the tectono-geochemistry weak information extraction method, highlighting the rationality of the deployment method, the representativeness of sampling points, the diversity of sampling media, and the validity (“yes” and “no”) of element anomalies and samples. Based on these, this study established the index system of this method. Finally, by combining the prospecting prediction of the eastern section of the Huijiabao anticline in the distribution area of Carlin-type gold deposits in southwestern Guizhou, this study concluded that the tectono-geochemistry weak information extraction method can extract the deep metallogenic weak information more effectively than the conventional tectono-geochemistry survey. It also inferred that this method has a good application prospect in the prospecting of concealed hydrothermal deposits and can be applied to the prospecting prediction of concealed hydrothermal deposits in all bedrock areas.

Key wordsbedrock area    hydrothermal deposit    prospecting prediction    tectono-geochemistry weak information extraction
收稿日期: 2021-09-04      修回日期: 2022-01-22      出版日期: 2022-12-20
ZTFLH:  P632  
基金资助:国家自然科学基金联合基金项目(U1812402);贵州省科技计划项目“贵州省卡林型金矿成矿与找矿科技创新人才团队建设”(黔科合人才平台-CXTD[2021]007);贵州省地质勘查资金项目“黔西南金矿多层次构造滑脱成矿系统研究与成矿预测”(520000214TLCOG7DGTDRG);贵州省研究生创新基金项目(黔教合YJSCXJH[2020]095)
通讯作者: 刘建中
作者简介: 宋威方(1992-),男,博士,主要从事卡林型金矿床成矿机制与找矿预测研究工作。Email:865770658@qq.com
引用本文:   
宋威方, 刘建中, 吴攀, 李俊海, 王泽鹏, 杨成富, 谭亲平, 王大福. 构造地球化学弱信息提取方法在黔西南卡林型金矿找矿中的应用[J]. 物探与化探, 2022, 46(6): 1338-1348.
SONG Wei-Fang, LIU Jian-Zhong, WU Pan, LI Jun-Hai, WANG Ze-Peng, YANG Cheng-Fu, TAN Qin-Ping, WANG Da-Fu. A successful application of the tectono-geochemistry weak information extraction method in the prospecting of Carlin-type gold deposits in southwestern Guizhou Province. Geophysical and Geochemical Exploration, 2022, 46(6): 1338-1348.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2022.1502      或      https://www.wutanyuhuatan.com/CN/Y2022/V46/I6/1338
Fig.1  矿致异常示意
Fig.2  构造地球化学弱信息提取方法采样点布置示意
1—主干断裂;2—次级断裂;3—节理和裂隙;4—背斜轴;5—节点位置及其采集点范围;6—采样点
Fig.3  构造地球化学弱信息提取采样介质示意
Fig.4  灰家堡背斜土壤地球化学测量Au、As、Sb、Hg元素异常[32]
1—嘉陵江组;2—夜郎组第三段;3—夜郎组第二段;4—夜郎组第一段;5—长兴组及大隆组;6—龙潭组第三段;7—地层界限;8—性质不明断层;9— 实测及推测正断层;10—实测及推测逆断层;11—背斜轴;12—向斜轴;13—超大型金矿床;14—金矿点;15—大型汞矿床;16—小型汞矿点;17—汞矿点;18—铊矿点;19—Au-As-Sb-Hg组合异常;20—矿体就位空间;21—金元素异常;22—砷元素异常;23—锑元素异常;24—汞元素异常
Fig.5  灰家堡背斜东段(者相金矿)Au、As、Sb、Hg、Tl元素异常[32]
1—嘉陵江组第三段;2—嘉陵江组第二段;3—嘉陵江组第一段;4—夜郎组第三段;5—夜郎组第二段;6—夜郎组第一段;7—地层界线;8—实测正断层及编号;9—实测逆断层及编号;10—性质不明断层;11—背斜轴;12—向斜轴;13—探矿权边界线;14—金元素异常;15—砷元素异常;16—锑元素异常;17—汞元素异常;18—铊元素异常;19—Au-As-Sb-Hg 组合异常
Fig.6  者相预测区深部钻探验证剖面[32]
1—永宁镇组第一段; 2—夜郎组第三段; 3—夜郎组第二段; 4—夜郎组第一段; 5—大隆组; 6—长兴组; 7—龙潭组第三段; 8—龙潭组第二段; 9—龙潭组第一段; 10—茅口组; 11—构造蚀变体(SBT); 12—断层; 13—矿体; 14—钻孔及编号
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