金厂沟梁金矿床地质特征及成因探讨  

Discussion on geologic character and genesis of deposit in Jinchanggouliang Gold Mine

作　　者：贾洪杰 张宝庆 蔡春杰 

机构地区：[1]内蒙古金陶股份有限公司,内蒙古赤峰024327

出　　处：《有色矿山》2001年第1期1-5,共5页Nonferrous Mines

摘　　要：金厂沟梁金矿床是内蒙古北部的大型金矿床 ,笔者对其地质特征及其成因做了探讨 ,认为矿床的成因与燕山期花岗岩体的侵入。Jinchanggouliang gold deposit is a large gold deposit in the north of Neimenggu. The geologic character and genesis of deposit are discussed in this paper, and the author think that ore genesis is related to the granitive intrusion during Yanshan period and Archaeozoic cosmic metamorphic rock system of high abundance gold.

关 键 词：地质特征 花岗闪长岩体 围岩 矿床成因 金矿床 岩浆岩 断裂构造 

分 类 号：P618.130.1[天文地球—矿床学]