| 大理州漾濞塔盘山锑-金矿床 |
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| 引用本文： | 杨世坤.大理州漾濞塔盘山锑-金矿床[J].云南地质,2008,27(1):53-58. |
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| 作者姓名： | 杨世坤 |
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| 作者单位： | 云南省有色地质楚雄勘查院,云南,楚雄,675000 |
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| 摘 要： | 以往工作对象是锑矿，伴生、独立存在的金矿未被重视。本文认为塔盘山锑、金矿床是富有机质的盆地热卤水以及古海水与深大断裂引起的韧性剪切带有关的低温变质热液改造矿床，有望找到中-大型金矿床。
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| 关 键 词： | 构造控矿 二期围岩蚀变 低溢厚度热液 锑金共生 塔盘山 漾濞云南 |
THE TAPANSHAN SB-AU DEPOSIT OF YANGBI, DALI |
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| YANG Shi-kun.THE TAPANSHAN SB-AU DEPOSIT OF YANGBI, DALI[J].Yunnan Geology,2008,27(1):53-58. |
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| Authors: | YANG Shi-kun |
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| Institution: | YANG Shi-kun ( Chuxiong Branch, Yunnan Nonferrous Institute of Geoexploration, Chuxiong 675000) |
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| Abstract: | The previous target is the Sb deposit, whereas people have not paid attention to the paragenetic Au with it. In this paper, we think that the Tapanshan Sb - Au deposit is the low T metamorphic hydrothermal reformation in relation to the ductile shear zone caused by macrofault, organic thermal brine and old seawater of basin, And we can expact a middle - large scale Au deposit will be discovered. |
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| Keywords: | Ore - Controlling of Structure 2 Periods of Wallrock Aheration Sb - Au Paragenesis Low T Metamorphic thermal fluid Tapanshan Yangbi Yunnan |
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