新疆吐鲁番市孔雀沟金矿地质特征  

Geological characteristics of peacock valley gold deposit in turpan,xinjiang

作　　者：窦祺枫 

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

出　　处：《世界有色金属》2017年第23期199-199,201,共2页World Nonferrous Metals

摘　　要：孔雀沟金矿位于南天山地向斜褶皱带的南缘。出露的主要赋矿地层为志留系乌勇布拉克群上亚群。矿体受北西-南东向的绢云母化、褐铁矿化及硅化的蚀变破碎带控制。孔雀沟金矿应属具有断裂破碎带控制的低温热液型金矿床。The Peacock GOLD gold deposit is located on the southern margin of the syncline fold belt in the southern Tianshan Mountains.Exposed to the main ore strata Silurian Wook Brak group on the sub-group.The ore bodies are controlled by northwest-south-east sericitization,limonite mineralization and silicified alteration and crushing zone.The peacock ditch gold deposit should belong to the low temperature hydrothermal gold deposit controlled by the fracture zone.

关 键 词：孔雀沟金矿 岩屑砂岩 蚀变破碎带 低温热液型金矿床 

分 类 号：P618.13[天文地球—矿床学] P631.81[天文地球—地质学]