湖南柏坊铜矿矿床地质特征及矿床成因初探

来源 :矿物学报 | 被引量 : 0次 | 上传用户:qingjietianjiao
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湖南省柏坊铜矿位于湖南省衡阳市,以小而富著称,包括铜鼓塘、刘家湾、柚子塘、大坪等矿段,矿化类型多样,矿体形态各异,成因复杂。前人对柏坊铜矿的矿床地质特征和同位素地球化学特征等方面开展了很多研究,马德成(2011)认为柏坊铜矿是原生沉积,后经地下热卤水淋滤再造的铜矿床。本文通过开展矿床地质特征研究,初步探讨矿床成因,以期为下步找矿工作提供资料指导。 The Parkfang Copper Mine in Hunan Province is located in Hengyang City, Hunan Province. It is known for being small and prosperous, including the Tongguntang, Liujiawan, Yuzuitang and Daping ore blocks. The mineralization types are diverse and the ore bodies are different in shape and complexity. Previous studies have carried out many studies on the geological characteristics and isotopic geochemical characteristics of the ore deposits in the Parkfontein copper mine. Madder (2011) argues that the Baofang copper deposit is a copper deposit that was originally deposited and then leached and reconstituted by underground heat brine. In this paper, through the study of the geological characteristics of the deposit, the genesis of the deposit is discussed tentatively so as to provide information guidance for the next prospecting work.
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