Geological Characteristics and Genesis of Wulonggou Gold Deposit and Evaluation of Gold Metallogenic Potential in East Kunlun  

作　　者：Yu Xuehui Department of Geology and Mineral Resources, China University of Geosciences, Beijing 100083 Mo Xuanzhi Architecture School, Yunnan University of Industry, Kunming 650051 Yuan Wanmen Institute of the Atom, Chinese Academy of Sciences, 

出　　处：《Journal of Earth Science》1999年第1期66-70,共5页地球科学学刊（英文版）

摘　　要：Wulonggou deposit is a large tectonoalteration gold deposit which is discovered in 1980s in East Kunlun area of Qinghai Province. The ore bodies occur in the rock series of metamorphic basement of Lower Proterozoic and granitoid Variscan to Lower Mesozoic. The shape, attitude and scale of the ore bodies are strictly controlled by the tectonoalteration belts, which show a typical characteristic of tectonoalteration deposits. A detailed discussion on typical deposits could also contribute to the evaluation of the regional gold metallogenic potential in East Kunlun area, and provide a direction for further gold prospecting between and/or near Kunzhong and Kunnan faults, and in areas of granitoid distribution of Variscan and Lower Mesozoic.Wulonggou deposit is a large tectonoalteration gold deposit which is discovered in 1980s in East Kunlun area of Qinghai Province. The ore bodies occur in the rock series of metamorphic basement of Lower Proterozoic and granitoid Variscan to Lower Mesozoic. The shape, attitude and scale of the ore bodies are strictly controlled by the tectonoalteration belts, which show a typical characteristic of tectonoalteration deposits. A detailed discussion on typical deposits could also contribute to the evaluation of the regional gold metallogenic potential in East Kunlun area, and provide a direction for further gold prospecting between and/or near Kunzhong and Kunnan faults, and in areas of granitoid distribution of Variscan and Lower Mesozoic.

关 键 词：tectonoalteration belt gold deposits East Kunlun Qinghai Province. 

分 类 号：P618.510.1[天文地球—矿床学]