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《Sichuan Nonferrous Metals》 2010-03
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The origin and metallogenic model of Gudongkeng fluorite deposit in Jinyun County,Zhejiang Province

FANG Yi,LI Zhong-quan(State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu610059,China)  
Geotectonically,the Gudongkeng fluorite deposit belongs to system of the southeastern part of Zhejiang province.It lies nearby the southeastern part of Yuyao-Suichang Presinianperiod metamorphosed basement upheaval,which is controlled by two NE trending deep fault,Jiangshan-Shaoxing deep fault and Yuyao-Lishui deep fault.The Gudongkeng fluorite deposit is controlled by formation and structure.The metallogenic material was from wall rock and the ore control major fault is NW-NWW-trending compressoshear faults.After many times field survey,combining the ore forming characteristics of territorial fluorite deposit,this text discussed the origin from three aspects of material source,water source and thermal source,discussed the forming process of ore solution in detail and established the metallogenic model to provide some reference for the exploration of the Gudongkeng fluorite deposit in the future.
【Fund】: 国家自然科学基金项目《托斯台伸展角度不整合与准噶尔盆地南缘成盆构造动力学研究》(编号:40773030);国家自然科学基金项目《龙门山前陆盆地南北段构造特征差异及成因机理研究》(编号:4057300)资助
【CateGory Index】: P619.215
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