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青海驼路沟地区钴(金)矿床赋矿地层与控矿构造特征
引用本文:唐健,王发明,许红英,李善平,张林.青海驼路沟地区钴(金)矿床赋矿地层与控矿构造特征[J].西北地质,2004,37(1):86-96.
作者姓名:唐健  王发明  许红英  李善平  张林
作者单位:1. 青海省地质调查院,青海,西宁,810012
2. 青海省地质矿产勘查开发局,青海,西宁,810001
基金项目:国土资源大调查项目(编号:200113000055)
摘    要:驼路沟地区钴(金)矿产找矿的突破,是近几年来国土资源大调查取得的重大成果。区内钴(金)矿床的空间定位与矿体展布受驼路沟-忠阳山复合型(或大型)韧性剪切带控制。矿床赋存于硫化物矿物相的沉积岩系中,显示了层控性的特点。矿区内岩石剪切变形明显,矿床类型为沉积改造型。

关 键 词:地层  构造  特征  驼路沟地区  青海  钴矿床  金矿床  赋矿地层  控矿构造特征
文章编号:1009-6248(2004)01-0086-11
修稿时间:2003年6月23日

Characteristics of ore-hosted strata and ore-controlling structure of Co-Au mineral deposit in Tuolugou area,Qinghai
TANG Jian,WANG Fa-ming,XU Hong-ying,LI Shan-ping,ZHANG Lin.Characteristics of ore-hosted strata and ore-controlling structure of Co-Au mineral deposit in Tuolugou area,Qinghai[J].Northwestern Geology,2004,37(1):86-96.
Authors:TANG Jian  WANG Fa-ming  XU Hong-ying  LI Shan-ping  ZHANG Lin
Institution:TANG Jian~1,WANG Fa-ming~1,XU Hong-ying~2,LI Shan-ping~1,ZHANG Lin~1
Abstract:The break-through in Co-Au mineral exploration in Tuolugou area,is a major achievement scored in the large-scale land resource survey in recent years. The special orientation of the Co-Au mineral deposit and distribution of its ore body is controlled by the loyal duetile shear zone of Tuolugou-Zhongyangshan.The mineral deposit occurred in the sedimental rock system of sulfide,shows the charactaristic of layer-controlled.Rocks underwent strongly shearing deformation.The mineral deposit type belongs to the sedimentary and transform one.
Keywords:strata  structure  characteristics
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