文章摘要
李厚民,胡正国.青海东昆仑驼路沟钴(金)矿床地质特征及成因初探[J].地质与勘探,2001,(1):60-64
青海东昆仑驼路沟钴(金)矿床地质特征及成因初探
GEOLOGY OF TUOLUGOU COBALT (GOLD) DEPOSIT IN EAST-KUNLUN MOUNTAINS, QINGHAI PROVINCE, AND THE FIRST DISCUSSION ON ITS GENESIS
  修订日期:2000-11-20
DOI:
中文关键词: 富钠火山岩 钴金矿床 矿床地质 成矿规律 动力变质变形作用
英文关键词: Tuolugou cobalt (gold) deposit, sodium volcanic rocks, kinetic metamorphism, east-KunLun Mountains, QingHai provinc
基金项目:国土资源部“九五”资源与环境科技攻关项目!(95 0 2 2 14 ),国土资源部定向科研项目!(95 -18),“九五”国家科技攻关30 5项目!(96-9
李厚民  胡正国
[1]中国科学院地质与地球物理研究所,北京100029 [2]长安大学,西安710054
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中文摘要:
      青海省格尔木市驼路沟钴(金)矿床是东昆仑地区新近发现的、国内外罕见的矿床新类型。笔通过研究首次认为该矿床形成于晚海西-印支-燕山期,为与富钠火山岩有关的层控-改造型独立钴(金)矿床,原富钠的中酸性火山岩中Co、Au初始富集,经后期动力变质变形作用改造成矿。
英文摘要:
      The Tuolugou cobalt (gold) deposit was first discoveried recently in East-KunLun district, Germu County, QingHai province. It is a new type of cobalt deposit in the world. We study this deposit and suggest that it was formed in late Variscian to Yinzhi-Yanshan epoch and that it is a independent strata-bound and remolding type cobalt deposit related to sodium volcanic rocks . Co, Au was first accumulated in this sodium-bearing intermediate-acid volcanic rocks and became cobalt (gold) deposit by the later kinetic metamorphism.
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