王宏,王疆丽,陈慕天,王吉勇,施美凤,朱华平.老挝川圹省PhuKham铜金矿床地质特征及找矿方向[J].地质找矿论丛,2014,29(1):66-71
老挝川圹省PhuKham铜金矿床地质特征及找矿方向
Geological characteristics and prospecting index of the PhuKham Cu-Au deposit in Xiangkhouang province, Laos
投稿时间:2013-04-11  修订日期:2013-10-11
DOI:10.6053/j.issn.1001-1412.2014.01.008
中文关键词:  Phu Kham 铜金矿  斑岩-夕卡岩型  地质特征  找矿方向  川圹省  老挝
英文关键词:PhuKham Cu-Au deposit  porphyry-skarn type  Geological characteristics  prospecting index  of ore Xiangkhouang  Laos
基金项目:中央地勘基金境外矿产资源风险勘查项目 (编号:[2011]D3-03)、中国地质调查局国土资源大调查项目 (编号:1212011220907;编号:1212011120337)联合资助。
作者单位
王宏 成都地质矿产研究所, 成都 610081 
王疆丽 成都地质矿产研究所, 成都 610081 
陈慕天 四川省地矿局成都水文地质工程地质中心, 成都 610081 
王吉勇 四川省地矿局402地质队, 成都 611730 
施美凤 成都地质矿产研究所, 成都 610081 
朱华平 成都地质矿产研究所, 成都 610081 
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中文摘要:
      老挝Phu Kham铜金矿为大型斑岩-夕卡岩型铜金矿床,地处老挝川圹省西南部。通过野外地质调查和室内工作,研究了Phu Kham铜金矿床形成的地质背景、矿床地质特征、成矿时代、找矿模式及成因类型。结果表明:铜金矿容矿岩系为石炭-二叠系碳酸盐岩、火山碎屑岩、夕卡岩及斑岩脉;矿石矿物主要为黄铁矿、黄铜矿、蓝铜矿、斑铜矿及孔雀石等;矿床成因为斑岩-夕卡岩型,成矿时代为晚石炭世—早二叠世。预测在Phu Kham矿区及长山成矿带内具有寻找大型-超大型铜金铁锡矿床的潜力。
英文摘要:
      PhuKham Cu-Au deposit is a large porphyry-skarn type Cu-Au deposit in southwest Xiangkhouang Province at central Laos. Field and Lab investigation and research reveal the geological and metallogenic background, characteristics of the metallogfewnic period, prospecting model and genetic type of the deposit. Host rock of the deposit includes Carboniferous-Permian carbonate rocks, volcanic clastic rocks, skarn and porphyry dyke. Pyrite, chalcopyrite, azurite, bornite and malachite are the main ore minerals. The deposit was formed in Late Carboniferous epoch-Early Permian epoch. According to its metallogenic model the Phu Kham deposit area and Changshan metallogenic belt are potential for prospecting large-super-large Cu-Au-Fe-Sn deposits.
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