摘要
杨山萤石矿赋存于合峪花岗岩基内,严格受控于构造破碎带,探明储量已达中型规模。本文通过矿床地质特征、围岩蚀变特征及成矿流体研究,认为杨山萤石矿应属构造充填的热液脉型萤石矿床。
Yangshan fluorite deposit occurs in Heyu granite base, strictly controlled by tectonic fracture zone, has proven reserves of medium-sized scal. According the study to the geological features, the alteration characteristics and the ore-forming fluids of Yangshan fluorite deposit, display Yangshan fluorite deposit have the obvious characteristics of the hydrothermal ore deposits.
作者
邓红玲
张苏坤
汪江河
刘耀文
冯绍平
张豪
王潇洒
黄岚
DENG Hong-ling ZHANG Su-kun WANG Jiang-he LIU Yao-wen FENG Shao-ping ZHANG Hao WANG Xiao-sa HUANG Lan(First Institute of Geological and Mineral Resources Survey, Henan Geological Exploration Bureau, Luoyang 471023, China Key Laboratory of Au-Ag-Polymetallic Deposit Series and Deep-seated Metallogenic Prognosis ofHenan, Luoyang 471023, China)
出处
《中国非金属矿工业导刊》
2017年第3期37-40,共4页
China Non-Metallic Minerals industry
基金
河南省国土资源科技攻关项目(编号:2015-258-03)
关键词
萤石矿床
地质特征
矿床成因
fluorite deposit
geological characteristics
deposit genesis
