会理县牛筋树—烂木桥蛇纹岩矿床地质特征及开发利用  

Geological characteristics and development and utilization of niujinshu lanmuqiao serpentine deposit in Huili County

作　　者：刘大生 LIU Da-sheng(geological team of Sichuan Bureau of Geology and mineral exploration and development,Xichang 615000,China)

机构地区：[1]四川省地质矿产勘查开发局四0四地质队,四川西昌615000

出　　处：《世界有色金属》2022年第13期124-126,共3页World Nonferrous Metals

摘　　要：矿体赋存于青龙山组(Pt1q):主要分布于尖山以北-白云村-大园子、菜园子-锅底塘、烂木桥一带,其岩性为:其岩性为碳钙质板岩、含粉砂碳质板岩、碳砂质板岩、白云石石英岩、含白云质微晶粉晶灰岩等.The ore body occurs in Qinglongshan formation (Pt1q):it is mainly distributed in the north of Jianshan-Baiyun Village-Dayuanzi,Caiyuanzi-guoditang,and lanmuqiao.Its lithology is:its lithology is carbon calcareous slate,silty carbon slate,carbon sandy slate,dolomite quartzite,dolomitic microcrystalline silty limestone,etc.

关 键 词：蛇纹岩 磁铁矿 开发利用 会理烂木桥 

分 类 号：P619.226[天文地球—矿床学]