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北祁连铜厂沟金矿地球化学特征与找矿标志研究
引用本文:刘军,肖荣阁,张汉成. 北祁连铜厂沟金矿地球化学特征与找矿标志研究[J]. 地质与勘探, 2006, 42(5): 34-38
作者姓名:刘军  肖荣阁  张汉成
作者单位:中国地质大学地质过程与矿产资源国家重点实验室,北京,100083;中国地质大学岩石圈构造、深部过程及探测技术教育部重点实验室,北京,100083;中国地质大学地质过程与矿产资源国家重点实验室,北京,100083;中国地质大学岩石圈构造、深部过程及探测技术教育部重点实验室,北京,100083;中国地质大学地质过程与矿产资源国家重点实验室,北京,100083;中国地质大学岩石圈构造、深部过程及探测技术教育部重点实验室,北京,100083
摘    要:文章根据铜厂沟金矿的矿区地质特征、碎屑岩岩石地球化学特征、英云闪长岩岩石化学特征、稀土元素地球化学特征等的研究,认为寒武纪碎屑岩原始沉积环境属于海洋岛弧优地槽环境复理石沉积物,复理石沉积物及超基性岩石为主要的矿源岩.提出英云闪长岩脉与超基性岩及绿泥石片岩边缘接触带中构造破碎带是有利的控矿构造部位,含黄铁矿硫化物石英脉是有利的找矿标志.

关 键 词:铜厂沟  金矿  稀土元素
文章编号:0495-5331(2006)05-0034-05
收稿时间:2005-08-24
修稿时间:2005-12-22

GEOCHEMICAL CHARACTERISTICS AND ORE PROSPECTING CRITERIA OF TONGCHANGGOU GOLD DEPOSIT, NORTHERN QILIAN
LIU Jun,XIAO Rong-ge,ZHANG Han-cheng. GEOCHEMICAL CHARACTERISTICS AND ORE PROSPECTING CRITERIA OF TONGCHANGGOU GOLD DEPOSIT, NORTHERN QILIAN[J]. Geology and Prospecting, 2006, 42(5): 34-38
Authors:LIU Jun  XIAO Rong-ge  ZHANG Han-cheng
Affiliation:1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083; 2. Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083
Abstract:Based on mine geology, petrology and geochemistry of clastic rock, tonalite petro - chemistry, and rare earth elements geochemistry in the Tongchanggou gold deposit, it is concluded that original sedimentary environment of Cambrian clastic rocks belongs to ocean island arc geosyncline environment flysch sediments and flysch sediments and uhrabasie rocks are main source of ores. It is pointed out that fractures in the contacting zone between tonalite and ultrabasic rocks or chlorite schist are favourable sites for ore - controlling. Pyrite - bearing sulfide quartz veins are favourable prospecting criteria.
Keywords:Tongchanggou   gold deposit   rare earth elements
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