| 赵杰,朱贤,胡绪云,梁永科,王德恭,唐志祥,黄小军,谢懿.湖南水口脚铜多金属矿地质特征及找矿研究[J].矿产勘查,2018,9(6):1145-1151 |
| 湖南水口脚铜多金属矿地质特征及找矿研究 |
| Geological characteristics and prospecting its’ prospects of copper polymetallic deposits in Shuikoujiao mining area, Hunan |
| 投稿时间：2017-10-20 |
| DOI： |
| 中文关键词: 水口脚铜多金属矿 地质特征 找矿前景 成矿规律 |
| 英文关键词: Shuikoujiao copper polymetallic deposit,geological characteristics,prospects,metallogenic regularity |
| 基金项目:湖南省级财政出资地质勘查项目湖南省江永县水口脚矿区铜矿普查(编号:20150342)资助。 |
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| 中文摘要: |
| 水口脚铜多金属矿处于南岭成矿构造带中段,水口山—铜山岭北东向壳断裂与都庞岭—铜山岭—九嶷山东西向基底断裂、怀化—道县北西向基底断裂的交汇地部位,矿床受北东东向构造及燕山期角闪石黑云母花岗闪长岩岩体控制。以往发现矿化体主要集中于中浅表,近年来通过深部钻探工作发现了新的铜矿体,找矿取得了突破。文章通过进一步研究矿床地质特征,总结成矿规律,分析找矿前景,以期对矿产勘查有所启示。 |
| 英文摘要: |
| Shuikou foot Copper Polymetallic Deposit, in the middle Nanling metallogenic tectonic belt, is located the junction of three faults such as the Shuikoushan-Tongshanling north east faults, the Dupangling-Tongshanling-Jiuyishan west east base fault and the Huaihua-Daoxian north west base fault, The deposit is controlled by the NEE structure and hornblende biotite granodiorite rocks in Yanshan period. Historical work show that the mineralized bodies found in the past mainly concentrated in shallow surface. But deep drilling work in recent years discovered new copper orebodies, which is a prospecting breakthrough. This paper further studied geological characteristics, summarized the metallogenic regularity and analyized the prospects expecting to provide some tips for exploration. |
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