云南地质
雲南地質
운남지질
YUNNAN GEOLOGY
2011年
3期
294-298
,共5页
层间破碎带锑矿%强硅化%上寒武统硅质岩%矿区外围可找矿前景%云南富宁里达
層間破碎帶銻礦%彊硅化%上寒武統硅質巖%礦區外圍可找礦前景%雲南富寧裏達
층간파쇄대제광%강규화%상한무통규질암%광구외위가조광전경%운남부저리체
Sb Deposit in Intrabed Fractured Zone%Strong Silicification%Upper Cambrian Silicic Rock%Prospecting Potentiality of Surrounding Area of Orefield%Lida,Funing,Yunnan
锑矿赋存于上寒武统博菜田组中段的硅质岩和硅化碳酸盐岩的层问破碎带中，矿化受区域上的北西向构造和地层所控制。深入研究，扩大资源和寻找新的资源基地。
銻礦賦存于上寒武統博菜田組中段的硅質巖和硅化碳痠鹽巖的層問破碎帶中，礦化受區域上的北西嚮構造和地層所控製。深入研究，擴大資源和尋找新的資源基地。
제광부존우상한무통박채전조중단적규질암화규화탄산염암적층문파쇄대중，광화수구역상적북서향구조화지층소공제。심입연구，확대자원화심조신적자원기지。
The Sb deposit is in the intrabed fractured zone of Upper Cambrian Bocaitian Formation Middle Member silicic rock and silicified carbonate rock. The metallogenesis is controlled by the regional NW- ward structure and strata. The extension of resources and prospecting of new resources can be carried out in the surrounding area of the orefield.
