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五台山区康家沟金矿床地质特征及找矿方向探讨
引用本文:张文亮,李朝辉,王亚丽.五台山区康家沟金矿床地质特征及找矿方向探讨[J].地质找矿论丛,2002,17(2):116-120.
作者姓名:张文亮  李朝辉  王亚丽
作者单位:冶金部第三地质勘查局,地勘院,山西,忻州,034000
摘    要:康家沟金矿属绿岩带型金矿。矿床(体)产于韧性剪切带中。NEE向构造为储矿(导矿)构造。矿床(体)由含金石英脉与其间蚀变岩组成。品位高低决定于含金石英脉的数量。含铁石英岩及其周围糜棱岩化带为近矿围岩。

关 键 词:绿岩带  韧性剪切带  含金石黄脉  地质特征  找矿方向  五台山区
文章编号:1001-1412(2002)02-0116-05
收稿时间:2001/12/17 0:00:00
修稿时间:2001年12月17

GEOLOGICAL CHARACTERISTICS OF KANGJIAGOU GOLD DEPOSIT AND ORE PROSPECT
ZHANG Wenliang,LI Zhaohui and WANG Yali.GEOLOGICAL CHARACTERISTICS OF KANGJIAGOU GOLD DEPOSIT AND ORE PROSPECT[J].Contributions to Geology and Mineral Resources Research,2002,17(2):116-120.
Authors:ZHANG Wenliang  LI Zhaohui and WANG Yali
Institution:Institute of the 3rd Geological and Exploration Burear, Xinzhou, 034000, China;Institute of the 3rd Geological and Exploration Burear, Xinzhou, 034000, China;Institute of the 3rd Geological and Exploration Burear, Xinzhou, 034000, China
Abstract:Kangjiagou Au deposit is a greenstone belt type deposit, controlled by shearing zone. NEN-trending structures are ore-locating structures. Ore bodies consists of Au-bearing quartz veins and the alteration rocks between them and ore grade depends on number of the quartz vein. The Au deposit is hosted in banded iron formation and in the surrounding mylonitized rock zone.
Keywords:greenstone belt  ductile shear zone  Au-bearing quartz vein  geological characteristics  ore-searching direction  Wutaishan area  
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