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青海省东昆仑夏日哈木矿区铜多金属矿床地质特征及控矿因素
引用本文:孔德岩,胡莹.青海省东昆仑夏日哈木矿区铜多金属矿床地质特征及控矿因素[J].青海大学学报,2014,32(6):63-66.
作者姓名:孔德岩  胡莹
作者单位:青海大学地质工程系,青海西宁,810016
摘    要:为了查明夏日哈木铜多金属矿床的控矿因素,从矿床的地质特征入手,同时采用光谱分析、氧化物分析以及贵金属分析等手段对矿石特征进行分析。从而总结出夏日哈木矿床类型属岩浆熔离型铜镍硫化物矿床,矿体主要受基性-超基性侵入岩控制。同时该矿床具有元古代大陆裂解时的成岩背景。

关 键 词:夏日哈木矿区  铜多金属矿床  地质特征  控矿因素

Geological characteristics and ore-controlling factors of the Xiarihamu copper polymetallic deposit
KONG Deyan,HU Ying.Geological characteristics and ore-controlling factors of the Xiarihamu copper polymetallic deposit[J].Journal of Qinghai University(Natural Science),2014,32(6):63-66.
Authors:KONG Deyan  HU Ying
Institution:( Department of Geological Erginecring, Qinghai University, Xining 810016, China)
Abstract:In order to find out the ore- controlling factors of Xiarihamu copper polymetallic deposit,the geological characteristics of ore deposit are analyzed. The ore characteristics are determined by analyzing spectrum of oxide as well as precious metal. The Xiarihamu deposit belongs to magmatic liquation copper- nickel sulfide deposits. The orebody is mainly controlled by the basic- ultrabasic intrusive rocks. The deposit has diagenetic background of continental rifting in Proterozoic era.
Keywords:Xiarihamu deposit  copper polymetallic deposit  geological characteristics  ore controlling factors
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