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云南麻栗坡洒西丫口白钨矿成矿规律
引用本文:许翠芳,舒培华,王建萍.云南麻栗坡洒西丫口白钨矿成矿规律[J].云南地质,2010,29(3):318-322.
作者姓名:许翠芳  舒培华  王建萍
作者单位:云南地矿资源股份有限公司文山分公司,云南,文山,663000
摘    要:晚志留世和白垩纪岩浆活动为成矿提供热源,碳酸盐岩为成矿提供化学反应场所、溶矿空间。圈出的3条白钨矿体以简单似层状沿Pt3s/Pt3n间构造面理(韧性剪切断裂带)产出,受Pt3s底部的层状矽卡岩(钙硅酸盐岩)控制。进一步工作,可望在接触带两侧找到理想白钨矿床。

关 键 词:高温热液成因  锡多金属白钨矿  岩体岩性控矿  沿构造面理产出  云南麻栗坡

THE METALLOGENESIS RULE OF SAXI SCHEELITE DEPOSIT IN MALIPO,YUNNAN
XU Cui-fang,SHU Pei-hua,WANG Jian-ping.THE METALLOGENESIS RULE OF SAXI SCHEELITE DEPOSIT IN MALIPO,YUNNAN[J].Yunnan Geology,2010,29(3):318-322.
Authors:XU Cui-fang  SHU Pei-hua  WANG Jian-ping
Institution:(Wenshan Branch,Yunnan Company(Ltd) of Geology & Mineral Resources,Wenshan 663000)
Abstract:The Late Silurian and Cretaceous magmatism provide the heat source.And the carbonate rock provides the place of chemical reaction and ore solution space.The 3 scheelite ore bodies have been outlined,which exist along the structural surface(ductility shear fault zone) between Pt3s/Pt3n in simple stratoid form,controlled by the bedded skarn(calcic silicate rock) of Pt3s bottom.We expect to discover the large scale scheelite deposit on the both sides of the contact in the future ore prospecting work.
Keywords:High T Hydrothermal Genesis  Sn Multimetallic Scheelite Deposit  Ore Control of Rock Body & Lithologic character  Occurrence along Structural Surface  Malipo  Yunnan
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