新疆特格里曼苏砂岩铜矿床地质特征及成因研究  

Geological characteristics and genesis of the sandstone deposit in the Xinjiang

作　　者：秦明辉 QIN Ming-hui(Fourth Geological Team of Hebei coalfield geology bureau,Xuanhua 075100,China)

机构地区：[1]河北省煤田地质局第四地质队,河北宣化075100

出　　处：《世界有色金属》2018年第18期92-93,共2页World Nonferrous Metals

摘　　要：特格里曼苏砂岩铜矿床位于北昆仑成矿带。矿体产于下石炭统库山河群碎屑岩地层中,大地构造位置上产于北昆仑晚古生代裂谷坳陷带内滨—浅海相红层建造中。矿体与围岩整合接触,呈似层状产出。该铜矿床属典型的同生层控砂岩型铜矿床。The Kunlun basin is located in the northern Kunlun metallogenic belt.Ore bodies occur in the clastic strata of the Kushanhe Group of Lower Carboniferous,and tectonically occur in the littoral-shallow marine red beds in the Late Paleozoic rift depression belt of North Kunlun.The contact between ore body and surrounding rock is similar to stratiform.The copper deposit is a typical synsedimentary sandstone hosted copper deposit.

关 键 词：铜矿床 地质特征 

分 类 号：P618.41[天文地球—矿床学]