青藏高原的金属矿产  

Metallic ore deposits on the Qinghai-Tibet Platea

作　　者：芮宗瑶[1] 李光明[2] 张立生[2] 王龙生[1] 王高明[2] 刘波[2] 

机构地区：[1]中国地质科学院矿产资源研究所,北京100037 [2]中国地质调查局成都地质矿产研究所,四川成都610082

出　　处：《中国地质》2006年第2期363-373,共11页Geology in China

基　　金：中国地质调查局地质大调查项目(2003 102 0008)资助

摘　　要：青藏高原地处印度板块与亚欧板块的衔接部位,长期处于岗瓦纳大陆边缘,大约在65 Ma时印度板块与亚欧板块发生碰撞,对过去构造格局和金属矿产等改造,同时产生新的构造格局和金属矿产,因此青藏高原的金属矿产别具一格。本文讨论青藏高原的铬、铁、铜钼、铅锌、锡、金、锑、铯等优势矿产。The Qinghai-Tibet Plateau lies in the junction between the Indian plate and Eurasian plate, on the northern margin of Gondwanaland. Collision of the Indian plate with the Eurasian plate about 65 Ma ago resulted in reworking of the tectonic framework and metallic ore deposits and also the formation of a new tectonic framework and new metallic ore deposits, which made metallic ore deposits on the Qinghai-Tibet Plateau distinctive. This paper deals with dominant mineral deposits of such metals as chromium, iron, copper-molybdenum, leadzinc, tin, gold, antimony and cesium on the Qinghai-Tibet Plateau.

关 键 词：青藏高原 金属矿产 印度板块 亚欧板块 

分 类 号：P617[天文地球—矿床学]