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.
出处
《有色矿山》
2001年第1期1-5,共5页
Nonferrous Mines
