云南元谋超基性岩群地质特征及综合开发探讨  

A DISCUSSION ON THE GEOLOGICAL FEATURE OF YUANMOU ULTRABASIC ROCK SWARMS IN YUNNAN PROVINCE AND THE COMPLEX DEVELOPING ON THEM

作　　者：薛步高 

机构地区：[1]云南省乡镇企业管理局

出　　处：《化工矿产地质》2000年第2期75-80,共6页Geology of Chemical Minerals

摘　　要：云南元谋超基性岩群中 ,朱布及黑泥坡以辉石橄榄岩为主 ,黑泥坡岩群中还有部分纯橄榄岩 ;白泥湾白铜厂为含镍蛇纹菱镁片岩。朱布、黑泥坡开发镁橄榄石砂、镁橄榄石砖与白铜厂开发水溶性农肥并副产菱镁矿均具良好的开发前景。In Zhubu and Heinipo there are mainly pyroxene peridotite ,there are also some pure peridotite in Heinipo rock swarm, in Bainiwan Baitongchang are Ni bearing sperpentine magnesite schist, among Yuanmuo ultrabasic rock swarms Yunan Province.There is a good prospect to develop forsterite sand and forsterite brick in Zhubu and Heinipo,develop water soluble fertilizer with magnesite byproduct in Baitongchang.

关 键 词：超基性岩体 镁砂 镁橄榄石砖 水溶性农肥 

分 类 号：P588.125[天文地球—岩石学]