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机构地区:[1]常山县国土资源局,浙江常山334200 [2]浙江省地质调查院,浙江杭州311203 [3]江西省地质矿产勘查开发局赣东北大队,江西上饶334000
出 处:《铜业工程》2008年第2期18-22,14,共6页Copper Engineering
摘 要:矿床地处扬子准地台华埠-新登陷褶带上方-罗村拗褶束西南段,矿床形成与二长花岗岩体和寒武纪灰岩紧密相关,矿体均位于岩前岩体与寒武纪灰岩接触带上,矿床规模大,矿石品位低,肉眼不易辨认,是近几年浙江省新发现的萤石矿床类型,对今后在本区域及相类似地区扩大找矿成果,开展勘查找矿具有重要指导意义。The Deposit locates at Yangzi Meta - platform Huabu - Upper of Xindengxian Ruche - Southwest of Luocun Niuzhesu. Its formation has close relationship with monzonitic granite and cambrian limestone. The orebody all locates on the contact zone of rock mass and cambrian limestone, with large scale, low grade and hard to make it out. It is one type of fluorite deposit which was found during the recent years in Zhejiang Province. It will be has great signification to extend prospecting and exploration in local and similar areas in the future.
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