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青海索拉沟银多金属矿床成矿特征及成因探讨
引用本文:何安全,李玉春,赵俊伟.青海索拉沟银多金属矿床成矿特征及成因探讨[J].吉林地质,2009,28(3):29-34.
作者姓名:何安全  李玉春  赵俊伟
作者单位:1. 青海省第三地质矿产勘查院,青海,西宁,810008
2. 青海省第五地质矿产勘查院,青海,西宁,8100012
摘    要:索拉沟地区位于青海省东昆仑东部与西秦岭造山带的接合部位,地质构造复杂,岩浆活动较强烈,成矿背景条件良好,是青海省贵金属、铜多金属重要的成矿带之一。根据矿床产出的地质构造环境、成矿特征、矿物组成、电子探针、流体包裹体温压测试及元素组合等特点分析,推测矿床的形成经历了热水沉积成矿和热液叠加改造成矿,索拉沟银多金属矿为热水沉积-热液叠加改造型。

关 键 词:青海索拉沟  银多金属  流体包裹体  矿床成因

Ore-forming characteristics and genesis of Suolagou silver polymetallic deposit, Qinghai Province
HE An-quan,LI Yu-chun,ZHAO Jun-wei.Ore-forming characteristics and genesis of Suolagou silver polymetallic deposit, Qinghai Province[J].Jilin Geology,2009,28(3):29-34.
Authors:HE An-quan  LI Yu-chun  ZHAO Jun-wei
Institution:HE An-quan, LI Yu-chun, ZHAO Jun-wei(1. Institute of the Third Geologic Exploration and Mineral Resources of Qinghai Province, Xining 810008, Qinghai, China; 2. Institute of the Fifth Geologic Exploration and Mineral Resources of Qinghai Province, Xining 8100012, Qinghai, China)
Abstract:The Suolagou area is located in the junction of eastern Kunlun Mountains in Qinghai Province and the west Qinling orogenic belt, showing complicated geological structure, relatively strong magmatic activities and a good metallogenetic setting, which is one of an important precious metal, copper-polymetallic metallogenic belt in Qinghai Province. According to geological tectonic setting, ore-forming, characteristics mineral composition, electron microprobe, temperature and pressure testing of fluid inclusions and characteristics of elements association, the forming of deposits undergone hydrothermal sedimentary mineralization and reformed mineralization,.Suolagou silver polymetallic deposit belongs to hydrothermal sedimentary-hydrothermal supraposition reformed one.
Keywords:Soulagou of Qinghai Province  silver polymetallic deposit  fluid inclusions  genesis of deposit
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