西藏江孜县热隆金银多金属矿床地质特征及成因初探  

PRELIMINARY STUDY ON GEOLOGY AND GENESIS OF RELONG POLYMETALLIC DEPOSIT OF GOLD AND SILVER IN JIANGZI COUNTY OF TIBET

作　　者：纪崇科 杜玉娥 魏东 

机构地区：[1]西安地质矿产勘查开发院,西安710100 [2]陕西省地质矿产勘查开发总公司,西安710154

出　　处：《陕西地质》2016年第2期14-20,共7页Geology of Shaanxi

摘　　要：热隆金银多金属矿床位于西藏自治区江孜县热隆一带,属北喜马拉雅Sb(As)、Pb、Zn、Au、Hg、Bi、Nb、Ta、Be、Cs白云母、水晶成矿带然巴—浪卡子变质核杂岩成矿远景区,矿体赋存于构造蚀变岩和石英脉中,受区内地层、构造、岩浆岩和变质作用共同作用。热隆金银多金属矿床为多期中低温热液型矿床。The polymetallic deposit of silver and gold is located in Relong area of Jiangzi County, Tibet Autonomous Region. It occurs in the mineralization area of Jamba - Langkazi metamorphosed core complex in the North Himalaya Sb （As）, Pb, Zn, Au, Hg, Bi, Nb, Ta, Be, Cs, mus- covite and crystal metallogenic belt. Affected by combined action of strata, structure, magmatic rocks and metamorphism, mineralized ore bodies occur in tectonic altered rocks and quartz veins. It is a multistage medium-low temperature hydrothermal deposit.

关 键 词：热隆 金银多金属矿 成矿地质特征 

分 类 号：P618.502[天文地球—矿床学]