摘要
察汗乌苏河地区位于青海省都兰县横跨祁漫塔格-都兰早古生代结合带和东昆北岩浆弧带。本文基于对青海省都兰-察汗乌苏河地区变质岩建造、火山岩建造、侵入岩建造、沉积岩建造特征的分析,总结了铜、铅、锌矿床的控制因素和成矿特点,讨论了区域建造构造与成矿作用的关系,为下一步深部找矿提供理论依据。
The Dulan-Qagan Us He area is located in south Qinghai Province, extending across the Early Paleozoic Qimantag-Dulan suture zone and the north East Kunlun magmatic arc. This paper deals with geological features and ore control factors of Cu, Pb, Zn deposits as well as relation of rock formation with mineralization on the basis of the features of metamorphic, volcanic, intrusive and sedimentary formation in the studied area.
出处
《四川地质学报》
2016年第2期187-190,194,共5页
Acta Geologica Sichuan
基金
中国地质调查局地质调查工作项目"四川攀枝花深部找矿疑难问题研究(1212011220867)"成都理工大学"里伍矿田控矿构造特征研究及隐伏矿体预测"联合资助
