芙蓉矿田北东向构造与矿床成因初探  

NE trending structure and genesis of Furong ore field

作　　者：王方有 WANG Fang-you(Southern Hunan Institute of Geology and Survey,Chenzhou 423000,China)

机构地区：[1]湖南省湘南地质勘察院,湖南郴州423000

出　　处：《世界有色金属》2020年第14期102-103,共2页World Nonferrous Metals

摘　　要：芙蓉矿田是国土大调查项目普查工作新发现的矿产地,其锡矿资源量已达特大型规模。文章通过大量的野外第一手资料,总结了芙蓉矿田基本地质特征,并对芙蓉矿田北东向构造进行了较详细分析,在现有勘查成果的基础上,结合矿体空间产出特征和矿体赋存状态,揭示了北东向构造与矿产的关系,对成矿规律和矿床成因进行了较深入的探讨,进一步明确了找矿方向。Furong Orefield is a newly discovered mining area in the general survey of the National Land University survey project,and its tin ore resources have reached a very large scale.Based on a large number of firsthand data in the field,this paper summarizes the basic geological characteristics of Furong Orefield,and makes a detailed analysis of the NE-trending structure of Furong Orefield.On the basis of the existing exploration results,combined with the spatial occurrence characteristics and occurrence state of orebodies,this paper reveals the relationship between NE-trending structures and minerals,makes a more in-depth discussion on the metallogenic regularity and deposit genesis,and further defines the prospecting direction.

关 键 词：芙蓉矿田 北东向构造 锡矿 矿床成因 

分 类 号：P612[天文地球—矿床学]