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新疆鄯善小尖山金矿区地质特征及控矿构造
引用本文:杨海兵.新疆鄯善小尖山金矿区地质特征及控矿构造[J].地质找矿论丛,2005,20(Z1):36-39.
作者姓名:杨海兵
作者单位:中国冶金地质勘查总局,西北地质勘查院,西安,710061
摘    要:小尖山金矿位于康古尔金矿中东段,矿体主要有含金蚀变岩和含金花岗细晶岩两类,以蚀变岩型金矿为主,发育于变质岩区,具有低温绿片岩相的面貌,受韧性剪切带控制并以剪切作用为主要的成矿机制.

关 键 词:小尖山金矿  蚀变岩型金矿  韧性剪切带  新疆
文章编号:1001-1412(2005)S0-0036-04
修稿时间:2005年4月21日

THE GEOLOGICAL CHARACTERISTICS OF XIAOJIANSHAN GOLD DEPOSIT IN SHANSHAN, XINJIANG AND ORE-CONTROL FACTOTRS
YANG Hai-bing.THE GEOLOGICAL CHARACTERISTICS OF XIAOJIANSHAN GOLD DEPOSIT IN SHANSHAN, XINJIANG AND ORE-CONTROL FACTOTRS[J].Contributions to Geology and Mineral Resources Research,2005,20(Z1):36-39.
Authors:YANG Hai-bing
Abstract:Xiaojianshan gold deposit is located the middle-east sector of Kangguer gold ore belt, there are two types of ore body, gold-bearing altered rock and gold-bearing granite-aplite. The deposit occur in metamorphosed rock, in which the gold-bearing altered rock type is dominant. The rock belongs to low greenschist facies. The deposit is controlled by a ductile shear zone. Shearing is the main ore-forming mechanism.
Keywords:Xiaojianshan gold deposit  altered rock type gold deposit  ductile shear zone  Xinjiang
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