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老挝琅勃拉邦帕奔矿区原生金矿床的地质特征及找矿方向
引用本文:刘禧超,张瑞华,车路宽.老挝琅勃拉邦帕奔矿区原生金矿床的地质特征及找矿方向[J].地质找矿论丛,2010,25(2):171-176.
作者姓名:刘禧超  张瑞华  车路宽
作者单位:天津华北地质勘查局地质研究所,天津,300170
摘    要:老挝帕奔金矿区位于区域性奠边府—琅勃拉邦断裂带的旁侧,受NE-NNE向韧脆性剪切带的控制,在下二叠系灰岩中产有构造破碎蚀变岩型金矿和含金方解石型脉金矿,全区分为6个矿化带,总体呈NNE向展布。金的富集受脆韧性断裂多次叠加或不同方向断裂交汇点的控制,矿化围岩中出现碳酸盐化、铁白云石化、菱铁矿化、大理岩化、高岭土化等热液蚀变。研究认为,区域上的韧脆性剪切带的延长部位应列为找矿区段,在灰岩和砂岩的接触地带(如M6矿化带西侧)应注意找矿,各矿化带内强片理化带的边部和构造的叠加、交汇部位是勘查工作的重点。

关 键 词:帕奔金矿  构造破碎蚀变岩型金矿  含金方解石脉型金矿  矿床地质特征  老挝
收稿时间:2010/5/13 0:00:00

GEOLOGICAL CHARACTERISTICS OF B.PHATEM PRIMARY GOLD DEPOSIT, LAOS AND THE ORE-SEARCHING DIRECTIONS
LIU Xichao,ZHANG Ruihua and CHE Lukuan.GEOLOGICAL CHARACTERISTICS OF B.PHATEM PRIMARY GOLD DEPOSIT, LAOS AND THE ORE-SEARCHING DIRECTIONS[J].Contributions to Geology and Mineral Resources Research,2010,25(2):171-176.
Authors:LIU Xichao  ZHANG Ruihua and CHE Lukuan
Institution:LIU Xi-chao,ZHANG Rui-hua,CHE Lu-kuan (Tianjin North China Non-ferrous Metal Geo-exploration Bureau,Tianjin 300171,China)
Abstract:B.Phatem primary gold deposit,Laos is located near the Dien Bien Phu-Luang Pracang fault belt and controlled by NE-NNE ductile-brittle shear zone.The altered cataclastic rock type Au ore and auriferous calcite veins occur in Permian limestone.In all there are 6 mineralization zones.Gold concentration is controlled by multi-overprinting of ductile-brittle fractures or intersection(superimposition) of fracture striking in different directions.Carbonation,ankeritization,sideritization,marblization and kaolitiz...
Keywords:B  Phatem gold deposit  the altered cataclastic rock type Au ore  auriferous calcite vein  the gold deposit geological characteristics  Laos  
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