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。
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.
出处
《云南地质》
2008年第1期53-58,共6页
Yunnan Geology
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
Ore - Controlling of Structure
2 Periods of Wallrock Aheration
Sb - Au Paragenesis
Low T Metamorphic thermal fluid
Tapanshan,Yangbi,Yunnan
