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新疆乔拉克金矿地质特征及成因分析
引用本文:曾晓建,谢春华.新疆乔拉克金矿地质特征及成因分析[J].矿产与地质,2001,15(Z1):457-463.
作者姓名:曾晓建  谢春华
作者单位:江西有色地质矿产勘查开发院
摘    要:乔拉克金矿产于伊什基里克晚古生代构造-岩浆岩带,从浅成-超浅成侵入体特征、断裂构造特征、蚀变分带和元素地球化学特征分析,认为矿床成因与强应变构造带及浅成-超浅成岩脉有密切关系,属于浅成中低温热液型金矿床,根据成矿地质特征,建立了找矿模式.

关 键 词:构造-岩浆岩带  地质特征  矿床成因  金矿  乔拉克  新疆
文章编号:1001-5663(2001)增刊-0457-07
修稿时间:2001年9月18日

Geologic characters of Qiaolake gold deposit of Xinjiang and its genetic analysis
ZENG Xiao jian,XIE Chun hua.Geologic characters of Qiaolake gold deposit of Xinjiang and its genetic analysis[J].Mineral Resources and Geology,2001,15(Z1):457-463.
Authors:ZENG Xiao jian  XIE Chun hua
Abstract:Qiaolake gold deposit occurs in Yishijilike later paleozoic tectonic magma rock belt.On the view of the characteristics of hypabyssal super hypabyssal intrusive,alteration zoning and element geochemistry,it is considered that the genesis of the deposit is closely associated with strong strain structure zones and hypabyssal super hypabyssal intrusive.It belongs to hypabyssal lower to mesothermal type gold deposit.An exploration model for the deposit has been built according to metallogenic characters.
Keywords:Tectonic  magmatite belt  Geological character  Ore genesis  Gold deposit  Qiaolake Xingjiang
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