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新疆也列莫顿地区小于赞浅成低温热液型金矿床地质地球化学
引用本文:徐国端.新疆也列莫顿地区小于赞浅成低温热液型金矿床地质地球化学[J].矿产与地质,1998(1).
作者姓名:徐国端
作者单位:贵州有色地质勘查局物化探总队
摘    要:小于赞金矿赋存于下石炭统大哈拉军山组陆相火山岩中,矿体受火山-次火山岩体与NW向断裂构造的联合控制,呈脉状产出。元素地球化学异常为Au-Ag-Hg-As-Bi组合。该矿床属浅成低温热液型金矿床。

关 键 词:金矿床,矿床地质地球化学,成矿过程,矿床成因,新疆,小于赞

GEOLOGY AND GEOCHEMISTRY OF XIAOYUZUAN EPITHERMAL LOW TEMPERATURE GOLD DEPOSIT IN YELIEMODUN DISTRICT OF XINJIANG AUTONOMOUS REGION
Xu Guoduan.GEOLOGY AND GEOCHEMISTRY OF XIAOYUZUAN EPITHERMAL LOW TEMPERATURE GOLD DEPOSIT IN YELIEMODUN DISTRICT OF XINJIANG AUTONOMOUS REGION[J].Mineral Resources and Geology,1998(1).
Authors:Xu Guoduan
Abstract:Xiaoyuzuan gold deposit occurs in the continental volcanic rocks in Dahalajunshan formation of Lower Carboniferous system.The orebodies,occurring in veins,are controlled by volcano subvolcanic rocks and northwest strike faults.The geochemical element anomaly is Au-Ag-Hg-As-Bi composition,The deposit belongs to epithermal low temperature type.
Keywords:Gold deposit  Geology and geoehemistry  Ore  forming process  Genesis of deposit  Xiaoyuzuan  Xinjiang
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