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湘南科学深钻构造样式及其对区域成矿预测的启示

刘阳生 赵正 文一卓 许若潮 李立兴 李厚民 许以明 田军委

矿床地质2024,Vol.43Issue(3):688-706,19.
矿床地质2024,Vol.43Issue(3):688-706,19.DOI:10.16111/j.0258-7106.2024.03.012

湘南科学深钻构造样式及其对区域成矿预测的启示

Structure styles of scientific deep drilling in South Hunan and implications for regional metallogenic prediction

刘阳生 1赵正 2文一卓 1许若潮 3李立兴 2李厚民 2许以明 1田军委1

作者信息

  • 1. 湖南省矿产资源调查所,湖南长沙 410014
  • 2. 中国地质科学院矿产资源研究所,北京 100037
  • 3. 湖南省矿产资源调查所,湖南长沙 410014||成都理工大学地球科学学院,四川成都 610000
  • 折叠

摘要

Abstract

The scientific deep drilling in south Hunan is located in the Baoshan mining area in Guiyang County,where is the middle section of intersection part of the Qin-Hang combinet belt and Nanling metallogenic belt,with the borehole end depth at 3008.93 m.A series of refined profiles/columns about lithology,structure,mineralization-related alteration,geochemistry and petrophysical properties were established based on detailed geological and geochemical drill-core record compiling and logging.The deep structures revealed by scientific deep drilling can be divided into three structural layers from the top to the bottom,including the upper(ductile)brittle structural layer mainly characterized by brittle fracture and followed by interlayer sliding and plastic deformation,the mid-dle brittle-ductile structural layer mainly showing bedding cambered seratification,and the lower ductile structur-al layer mainly displaying plastic deformation and followed by interlayer sliding and plastic shear.The deep struc-ture is represented by the north-east Yanling-Chenzhou-Linwu deep fault belt.The intense Yanshanian activity in-duced magma emplacement to the hanging wall of the deep fault(northwest part of the deep fault),resulting in formation of the Baoshan-Dafang granodiorite porphyry dyke belt and associated Cu-Pb-Zn-Ag-Au deposit,the Huangshaping quartz porphyry dyke swarm and associated Pb-Zn-Ag deposit,and the Huangshaping granite por-phyry dyke swarm and associated W-Sn-Mo-Pb-Zn deposit.The δ34S values of the sulfide ore samples collected from the tunnel and deep drill core indicate that the sulfur of skarn-type Cu-Pb-Zn deposit sourced from magma,whereas sulfur of the vein-type Pb-Zn-Ag deposit sourced from a mixture of magma and strata.Combining the da-ta of deep structure,magma emplacement and geophysics,three exploration target areas are proposed:the depth more than-1350 m in the central region of Baoshan has potential for exploration of skarn-type Cu ores;the Mis-haijing area between the Baoshan area and Dafang area has good potential for exploration of northeast-extending vein-like Pb-Zn-Ag-Au ores;The Huangshasi mining area may have a hidden granodiorite porphyry body and granite porphyry body in the deep part,which may be a prospecting target for W-Sn-Mo-Bi-Cu-Pb-Zn ores.

关键词

湘南科学深钻/构造样式/找矿靶区/钦杭结合带

Key words

scientific deep drilling in South Hunan/prospecting target/Qinzhou-Hangzhou Bay orogenic juncture belt

分类

天文与地球科学

引用本文复制引用

刘阳生,赵正,文一卓,许若潮,李立兴,李厚民,许以明,田军委..湘南科学深钻构造样式及其对区域成矿预测的启示[J].矿床地质,2024,43(3):688-706,19.

基金项目

本文得到国家重点研发计划项目重点专项(编号:2018YFC0603905、2022YFC2905101)和湖南省地质院院本级科研项目(编号:HNG-STP202204)联合资助 (编号:2018YFC0603905、2022YFC2905101)

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