摘要
崇义塘漂孜钨矿产于张天堂燕山期中细粒斑状二云母花岗岩顶部细粒斑状白云母花岗岩中,矿体出露地表,矿床的形成与细粒、似斑状酸性岩浆岩有关,并与花岗岩自蚀变作用白云母化、钠长石化等关系密切。成矿物质主要源于陆壳重熔型岩浆岩,矿床成因类型为白云母化、钠长石化蚀变花岗岩亚型(变花岗岩型)。塘漂孜岩体型钨矿床的发现,对本区同类矿床找矿具有理论和现实指导意义,可进一步在赣南拓展钨多金属矿的找矿空间。
Tangpiaozi granite body-type tungsten deposit occurred in the fine grain porphyritic white mica granite at the top of middle fine grmn porphyritic two-mica granites ot the Yanshan Zhangtiantang rock body. The ore body exposed on the surface. The ore deposit formation is related with the fine grain,porphyritic acidic magmatic rock ,and associated with the granite, alliteration metallogenic materials are derived from continental crust remehing magmatic rocks. The discovery of Tangpiaozi tungsten deposit has the ore prospecting significance in searching the similar ore deposits in the area.
出处
《资源调查与环境》
2006年第2期153-158,共6页
Resources Survey & Environment
关键词
岩体型钨矿床
地质特征
找矿意义
塘漂孜
江西
granite body-type tungsten deposit
geological characteristics
prospecting significance
Tangpiaozi
Chongyi county of Jiangxi province
