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黄金科学技术 ›› 2023, Vol. 31 ›› Issue (3): 433-442.doi: 10.11872/j.issn.1005-2518.2023.03.151

• 矿产勘查与资源评价 • 上一篇    下一篇

贵州贞丰县卡务地区金矿地质特征与找矿预测

王大福1(),刘建中2,3,4(),王泽鹏1,3,陈发恩1,杨成富1,3,徐良易1,4,李俊海1,3,刘婧珂1,潘启权1,龙成雄1,汪小勇1   

  1. 1.贵州省地质矿产勘查开发局一〇五地质大队,贵州 贵阳 550018
    2.贵州省地质矿产勘查开发局,贵州 贵阳 550004
    3.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
    4.贵州大学,贵州 贵阳 550025
  • 收稿日期:2022-10-19 修回日期:2022-12-05 出版日期:2023-06-30 发布日期:2023-07-20
  • 通讯作者: 刘建中 E-mail:748983010@qq.com;2585364825@qq.com
  • 作者简介:王大福(1989-),男,贵州开阳人,硕士研究生,从事矿产地质勘查研究工作。748983010@qq.com
  • 基金资助:
    国家自然科学基金项目“我国西南(贵州)喀斯特地区特色矿产成矿理论及综合利用”(U1812402);国家重点研发计划“深地资源勘查开采”重点专项“深部矿产资源三维找矿预测评价示范”(2017YFC0601500);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”(编号:黔科合平台人才-CXTD[2021]007)和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找矿预测”(520000214TLCOG7DGTNRG)

Geological Characteristics and Prospecting Prediction of Gold Deposit in Kawu Area,Zhenfeng County,Guizhou Province

Dafu WANG1(),Jianzhong LIU2,3,4(),Zepeng WANG1,3,Fa’en CHEN1,Chengfu YANG1,3,Liangyi XU1,4,Junhai LI1,3,Jingke LIU1,Qiquan PAN1,Chengxiong LONG1,Xiaoyong WANG1   

  1. 1.No. 105 Geological Team, Bureau of Geology and Mineral Exploration and Development Guizhou Province, Guiyang 550018, Guizhou, China
    2.Bureau of Geology and Mineral Exploration and Development Guizhou Province, Guiyang 550004, Guizhou, China
    3.Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550081, Guizhou, China
    4.Guizhou University, Guiyang 550025, Guizhou, China
  • Received:2022-10-19 Revised:2022-12-05 Online:2023-06-30 Published:2023-07-20
  • Contact: Jianzhong LIU E-mail:748983010@qq.com;2585364825@qq.com

摘要:

为进一步识别卡务地区金矿新的找矿标志,开展了找矿预测工作。首先,通过对卡务地区进行野外地质调查,开展研究区地质背景和典型矿床地质特征的深入研究,新识别出区内岩石能干性差异大的岩层界面之间存在构造蚀变体(SBT),且金矿体主要赋存于SBT和背斜近轴部的高角度逆断层及层间破碎带中;然后,通过系统总结卡务地区金矿成矿要素,发现其成矿地质特征与新寨金矿基本一致,认为卡务地区金矿与区域卡林型金矿属于同一成矿系统;最后,基于黔西南金矿多层次构造滑脱成矿系统和找矿预测模型,开展了找矿预测,圈定找矿预测区3个,预测卡务地区潜在金资源量为50 t。

关键词: 卡林型金矿, 构造蚀变体, 控矿因素, 找矿预测, 卡务地区, 贵州省

Abstract:

The tectonic position of the study area belongs to the junction of the southwest edge of the Yangtze quasi platform and the Youjiang fold belt of the south China fold belt,which is an important component of carlin-type gold deposits area in southwest Guizhou.The deep hidden deposit prospecting has not made a new breakthrough.Based on the recent research on structure-controlled alteration zone (SBT) and the latest theoretical results of multi-level structural slippage metallogenic system of carlin-type gold deposits in Nanpanjiang-Youjiang area,the geological background and geological characteristics of typical deposits are studied through field investigation in the Kawu,Southwestern Guizhou,China.The results further clarified the geological characteristics of gold deposits in the Kawu area and identified the main prospecting criteria,established the core elements of gold prospecting prediction in the Kawu area,and newly identified the existence of SBT between the rock interfaces with large differences in rock competence in the area,providing an important basis for regional prospecting prediction.The gold orebody is deposited in SBT and the high-angle pressure fault and the interlayer fracture zone,system summary Kawu area gold metallogenic elements.The study shows that the regional structural detachment and interlayer fracture zone are the main channel of metallogenic fluid migration and the ore site of gold ore body,the abnormal overlap parts of the metallogenic elements such as Au,As,Sb and Hg are the most favorable parts of mineralization,which is the same metallogenic system as the regional carlin-type gold deposit,and the gold metallogenic conditions are superior.Based on the multi-level structural detachment metallogenic system and the prospecting prediction model,the prospecting prediction was carried out,3 prospecting prediction areas were delineated,the gold resources in Kawu area were predicted as 50 t,and the prospecting direction in the area is defined,so as to provide guidance and reference for the subsequent prospecting work in this area.

Key words: carlin-type gold deposit, structure alteration rocks (SBT), ore-controlling factor, prospecting prediction, Kawu area, Guizhou Province

中图分类号: 

  • P618.51

图1

卡务地区地质矿产简图1.中三叠统边阳组;2.中三叠统许满组;3.中三叠统新苑组;4.中—下三叠统罗楼组;5.中—下三叠统乐康组;6.上二叠统吴家坪组;7.中—上二叠统领薅组;8.中二叠统猴子关组;9.中—下二叠统四大寨组;10.古近纪钙碱性煌斑岩;11.构造蚀变体及界线;12.地层界线;13.逆断层;14.性质不明断层;15.背斜;16.倒转背斜;17.向斜;18.产状;19.小型金矿床;20.金矿点"

图2

卡务金矿构造蚀变体剖面示意图1.中—上二叠统领薅组二段;2.中—上二叠统领薅组一段;3.中—下二叠统四大寨组;4.黏土质粉砂岩;5.砂岩;6.黏土岩;7.灰岩;8.角砾岩;9.岩屑;10.砾屑;11.硅化;12.黄铁矿化;13.地层界线;14.构造蚀变体及界线;15.金矿体"

图3

卡务金矿构造蚀变体蚀变特征"

表1

卡务地区金矿成矿要素"

成矿要素主要特征
成矿地质体燕山期隐伏花岗岩体(110~150 Ma)
成矿构造及成矿结构面成矿构造:白层背斜、卡务背斜、包树背斜、滑脱构造以及与背斜同期形成的逆断层;成矿结构面:断裂面、背斜轴面、灰岩与黏土岩(粉砂岩)界面以及玄武岩与凝灰岩界面
结构类型“断裂+构造蚀变体(SBT)”的上、下二元结构模式
成矿作用特征标志成矿早阶段:石英—白云石阶段(玉髓+石英+白云石);成矿主阶段:黄铁矿—毒砂阶段(黄铁矿+毒砂);成矿晚阶段:石英—方解石阶段(方解石+石英)

图4

中国南方卡林型金矿多层次构造滑脱成矿系统示意图(刘建中等,2022)1.花岗岩体;2.断裂;3.构造蚀变体;4.金矿体;5.大气降水;6.地层水;7.变质水;8.岩浆水"

表2

卡务地区卡林型金矿找矿预测核心要素"

典型矿床构造构造特征构造蚀变体成矿范围
翼间角轴面倾角轴倾伏角厚度/m岩石组合
卡务金矿床卡务背斜100°~140°60°~90°5°~20°2~20

上:细碎屑岩(P2-3lh);

下:灰岩(P1-2sd

背斜轴附近2 000 m
新寨金矿床白层背斜100°~160°80°~90°5°~20°未发现未发现背斜轴附近1 500 m、断裂带深部延伸
典型矿床

成矿面积

/ km2

矿床规模/tSBT中矿体规模成矿背景成矿条件成矿要素地球化学特征
卡务金矿床300.26长:30~100 m;宽:20~50 m黔西南金矿集区赖子山矿田北段卡务背斜及断裂构造、SBT、岩性组合、热液蚀变Au、As、Sb、Hg
新寨金矿床152.83未发现黔西南金矿集区赖子山矿田北段白层背斜(穹隆)及断裂构造、SBT、岩性组合、热液蚀变Au、As、Sb、Hg

表3

卡务地区卡林型金矿预测区块"

预测区

名称

预测要素面积/km2预测延深/m预测埋深/m查明金资源量/t预测潜在金资源量/t
合计644

卡务

预测区

成矿构造:卡务背斜;成矿结构面:P2-3lh/P1-2sd构造蚀变体(SBT)、断裂;赋矿地层:P2-3lh;容矿岩石:构造角砾岩、玄武质岩屑砂岩、凝灰质黏土岩、粉砂岩;矿体类型:层控为主,断控为辅;热液蚀变:硅化、黄铁矿化、毒砂化、褐铁矿化、方解石化和白云石化;已有矿床(点):卡务;矿体埋深:100~500 m25.832 000100~500120

新寨

预测区

成矿构造:白层背斜、断裂;成矿结构面:T1-2l/P3w构造蚀变体(SBT)、断裂;赋矿地层:T1-2l、T2x和T2b;容矿岩石:构造角砾岩、钙质砂岩、钙质粉砂岩和黏土质粉砂岩;矿体类型:层控、断控;热液蚀变:硅化、黄铁矿化、褐铁矿化、方解石化、白云石化和黏土化;已有矿床(点):新寨;矿体埋深:100~500 m14.641 800100~500510

包树

预测区

成矿构造:包树背斜;成矿结构面:T1-2l/P3w之间构造蚀变体(SBT);赋矿地层:T1-2l;容矿岩石:钙质粉砂岩和泥灰岩;矿体类型:层控;热液蚀变:硅化、黄铁矿化、褐铁矿化和方解石化;已有矿床(点):包树;矿体埋深:100~300 m10.661 000100~300014

图5

卡务地区卡林型金矿预测分布图1.逆断层;2.性质不明断层;3.背斜;4.倒转背斜;5.向斜;6.成矿预测区"

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