新疆伊宁县吐拉苏盆地金多金属调查分析  

Yining county, xinjiang spit gold polymetallic survey he basin analysis

作　　者：韩波涛 

机构地区：[1]新疆维吾尔自治区有色地质勘查局七0一队,新疆乌鲁木齐831100

出　　处：《世界有色金属》2017年第2期249-250,共2页World Nonferrous Metals

摘　　要：新疆伊宁县吐拉苏盆地金多金属成矿带所处大地构造位置属于博罗科努早古生代岛弧的西段。该成矿区域属于浅成低温热液型斑岩型金多金属成矿,金矿床成矿物质来源为岩浆岩及蓟县系、奥陶系和志留系地层,岩浆岩也是该区域为金的来源之一。Yining county, xinjiang spit gold polymetallic metallogenic belt he basin the geotectonic position is owed rocco＇s early Paleozoic arc fault.The metallogenic area belongs to hypabyssal low temperature hydrothermal type porphyry gold polymetallic mineralization, gold deposit ore-forming material sources for magmatic rocks and jixian system, the ordovician and silurian strata, magmatic rocks and the region as a source of gold.

关 键 词：金多金属成矿带 矿床特征 成矿分析 

分 类 号：P618.42[天文地球—矿床学]