老挝琅勃拉邦爬奔金矿矿床地质及成因探讨
로과랑발랍방파분금광광상지질급성인탐토
A PROBE INTO THE GEOLOGY AND GENESIS OF PHAPON AU DEPOSIT IN LUANGPRABANG, LAOS
  • 万方数据
    云南地质 운남지질
    YUNNAN GEOLOGY
    2011年 3期 280-284 ,共5页

    李会恺%张翔君%王军

    리회개%장상군%왕군

    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 低溫熱液型金礦%剪切帶控製%灰巖礦源層%下二疊統%老撾爬奔
    저온열액형금광%전절대공제%회암광원층%하이첩통%로과파분
    Low T Hydrothermal Au Deposit%Control of Shear Zone%Limestone Ore Source Bed%LowerPermian%Phapon,Laos
    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。
    랑발랍방성위우“삼강”성광대남연부분，파분금광위수전절대공제적저온열액광상，광체산출공간부합리덕이전절렬극규률，진일보공작후해광구응유중형이상규모。
    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.
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