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老挝琅勃拉邦爬奔金矿矿床地质及成因探讨
引用本文:李会恺,张翔君,王军.老挝琅勃拉邦爬奔金矿矿床地质及成因探讨[J].云南地质,2011,30(3):280-284.
作者姓名:李会恺  张翔君  王军
作者单位:1. 天津华北地质勘查总院,天津,300181
2. 天津华北地质勘查局,天津,300181
摘    要:琅勃拉邦省位于“三江”成矿带南延部分,爬奔金矿为受剪切带控制的低温热液矿床,矿体产出空间符合里德尔剪切裂隙规律,进一步工作后该矿区应有中型以上规模。

关 键 词:低温热液型金矿  剪切带控制  灰岩矿源层  下二叠统  老挝爬奔

A PROBE INTO THE GEOLOGY AND GENESIS OF PHAPON AU DEPOSIT IN LUANGPRABANG, LAOS
LI Hui-kai,ZHANG Xiang-jun,WANG Jun.A PROBE INTO THE GEOLOGY AND GENESIS OF PHAPON AU DEPOSIT IN LUANGPRABANG, LAOS[J].Yunnan Geology,2011,30(3):280-284.
Authors:LI Hui-kai  ZHANG Xiang-jun  WANG Jun
Institution:LI Hui-kai1,ZHANG Xiang-jun1,WANG Jun2(1.North China Geoexploration Institute General,Tianjin 300181)(2.North China Geoexploration Bureau,Tianjin 300181)
Abstract:Luangprabang is the S -ward extension Au deposit is a low T hydrothermal deposit controlled by with Lider shearing fracture rule, By the further work, area of "Three - River" metallogenetic zone. The Phapon the shear zone. The space of ore body is in concordance the orefield scale must be more than medium size.
Keywords:Low T Hydrothermal Au Deposit  Control of Shear Zone  Limestone Ore Source Bed  LowerPermian  Phapon  Laos
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