川西南康定—会理地区构造演化与金矿成矿  

THE TECTONIC EVOLUTION AND GOLD MINERALIZATION FROM KANGDING TO HUILI,SOUTHWEST OF SICHUAN

作　　者：葛良胜[1,2] 李玉静 郭晓东[1] 邹依林[1] 

机构地区：[1]黄金地质研究所 [2]河北地质学会

出　　处：《黄金地质》1998年第3期7-14,共8页Gold Geology

摘　　要：从区域大地构造演化的角度阐述了研究区金矿成矿的大地构造环境，并依据其对金矿成矿的控制，划分了金矿大地构造成矿区（带），分析了不同区（带）内金矿成矿特征。通过讨论不同大地构造演化阶段及不同构造体制与金矿成矿的关系，阐述了区域金矿成矿的时空特征。The geotectonic enviroment of gold mineralization in the research area is illustrated from the angle of regional geotectonic evolution. The geotectonic mineralization zones of gold are divided and the ore forming characteristics of gold deposit in different zones are analysed. The space time characteristics of regional gold mineralization are illustrated by discussing the relation of different tectonic systems and gold mineralization in different geotectonic evolution stages.

关 键 词：板块构造环境 成矿作用 构造演化 四川 金矿床 

分 类 号：P618.510.5[天文地球—矿床学] P547[天文地球—地质学]