都娘山—扎合地质特征与热液型矿床成因关系  

Geological characteristics and the genesis of hydrothermal type deposit in Duniang mountain-zhahe

作　　者：李功振 丁啸 

机构地区：成都理工大学构造成矿成藏重点实验室,四川成都610059

出　　处：《世界有色金属》2016年第6期203-203,205,共2页World Nonferrous Metals

摘　　要：都娘山位于达日县城到桑日麻一带。该区发育一系列的北西向断裂和复式褶皱,区内1：20万化探圈定的异常区与构造关系明显。本文以构造-热液型矿床成矿系列的思路,通过对地层、断裂和褶皱以及岩浆岩开展成矿条件、成矿特征和成矿控制因素研究,总结成矿规律,对区域找矿前景做出评价。Both the mother mountain is located in the county to the sangrima dari area. The development of a series of NW trending faults and folds, the relationship between 1：20 and abnormal zone area exploration and construction of the clear delineation. The tectonic hydrothermal metallogenic series of train of thought by the strata, faults and folds and magmatic rocks carry out metallogenic conditions and metallogenic characteristics and controlling factors of, summarization of metallogenic regularities, to the regional prospecting prospect evaluation.

关 键 词：热液矿床 都娘山 扎合 

分 类 号：P618.4[天文地球—矿床学]