中国地质2011，Vol.38Issue(3)：673-680,8.
云南麻栗坡南秧田白钨矿床层控似矽卡岩成因探讨
The genesis of skarnoid from the Nanyangtian stratabound scheelite deposit in Malipo, Yunnan Province
摘要
Abstract
The Nanyangtian scheelite ore deposit is a rarely-seen layered scheelite deposit in southeastern Yunnan,whose ore body is hosted in the layered skarnoid of Proterozoic Nanyangtian Rock Group. Based on detailed field work in combination with indoor rock geochemical analysis as well as a comparison with typical ore deposits both in China and abroad, the authors carried out restoration of original rock of skarn,found that the original rock of the skarn seems to be submarine volcanic eruption (or hot water) sediments combined with terrigenous clastic rocks, and reached the conclusion that the skarn was metasedimentary skarn belonging to skarnoid.关键词
南秧田/层状似矽卡岩/成因/沉积变质Key words
Nanyangtian/ layered skarnoid/ genesis/ metasediment分类
天文与地球科学引用本文复制引用
石洪召,张林奎,任光明,刘书生,张彬,戴婕,陈敏华..云南麻栗坡南秧田白钨矿床层控似矽卡岩成因探讨[J].中国地质,2011,38(3):673-680,8.基金项目
地质调查"云南麻栗坡地区矿产远景调查"项目(1212010880402)资助. （1212010880402）
