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楚雄南华大龙塘金矿控矿因素新知
引用本文:何云,杨丽兰,周红升.楚雄南华大龙塘金矿控矿因素新知[J].云南地质,2008,27(4):448-454.
作者姓名:何云  杨丽兰  周红升
作者单位:云南地矿博泰矿业有限责任公司,云南,昆明,650200
摘    要:“大龙塘式”金矿模式地位于红河断裂以西的哀牢山造山带的后陆盆地,山麓河流相含Au、Ag等成矿元素及自然金磨拉石沉积建造,燕山期NW向断裂控矿,为层控砂砾岩地下水中低温热液改造型金矿。

关 键 词:控矿因素  成矿规律  找矿远景  大龙塘金矿  云南南华

THE NEW KNOWLEDGE OF METALLOGENESIS CONTROLLING FACTORS OF DALONGTANG AU DEPOSIT OF NANHUA, CHUXIONG
HE Yun,YANG Li-lan,ZHOU Hong-sheng.THE NEW KNOWLEDGE OF METALLOGENESIS CONTROLLING FACTORS OF DALONGTANG AU DEPOSIT OF NANHUA, CHUXIONG[J].Yunnan Geology,2008,27(4):448-454.
Authors:HE Yun  YANG Li-lan  ZHOU Hong-sheng
Institution:( Botai Mining Company of Yunnan, Kunming 650200)
Abstract:The "Dalongtang type" Au deposit is located in the backland basin of Ailaoshan Orogen west of Honghe fault.The main metallogenesis controlling factors are the ore-forming elements Au,Ag,etc,of piedmont-river facies,native Au molasse sedimentary formation and Yanshanian NW fault,which belongs to the Au deposit of stratabound underground water middle-low T hydrothermal reformed type of psepholite.
Keywords:Metallogenesis Controlling Factor  Metallogenetic Rule  Prospecting Potentiality  Dalongtang Au Deposit  Nanhua  Yunnan
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