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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
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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.
作者 王方有 WANG Fang-you(Southern Hunan Institute of Geology and Survey,Chenzhou 423000,China)
出处 《世界有色金属》 2020年第14期102-103,共2页 World Nonferrous Metals
关键词 芙蓉矿田 北东向构造 锡矿 矿床成因 Furong Orefield NE trending structure tin deposit deposit genesis
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