地质学
泥盆纪
前寒武纪
地球化学
二叠纪
硅质碎屑
克拉通
古生物学
裂谷
岩性
古生代
碳酸盐岩
构造盆地
沉积岩
沉积沉积环境
构造学
作者
Wenchao Su,Wendou Dong,Xing-Chun Zhang,Nengping Shen,Ruizhong Hu,Albert H. Hofstra,Lianzheng Cheng,Yong Xia,Keyou Yang
摘要
The Dian-Qian-Gui "Golden Triangle" area of southwest China has the second-largest concentration of Carlin-type gold deposits in the world, containing more than 800 tonnes of Au (25.7 Moz). All of the deposits are located along long-lived, deep-penetrating crustal structures inherited from Devonian rifting of the Precambrian Yangtze craton. They are hosted in Cambrian to Middle Triassic platform carbonate, transitional, and siliciclastic rocks of the Youjiang basin, and locally in Late Permian diabase intrusions or volcaniclastic rocks. These deposits have many characteristics in common with Carlin-type gold deposits in Nevada, USA, including lithology of host rocks, alteration types, elemental associations, and occurrence of gold.
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