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银虎曼铅-锌矿床地质特征、矿床成因及找矿标志
引用本文:谢国敏,杨士辉,谢珂.银虎曼铅-锌矿床地质特征、矿床成因及找矿标志[J].矿产与地质,2007,21(5):546-550.
作者姓名:谢国敏  杨士辉  谢珂
作者单位:河南省地质矿产勘查开发局第一地质勘查院,河南,南阳,473003
摘    要:银虎曼铅-锌矿床地处万沟多金属成矿带东段。二郎坪群火神庙组中PPb、Zn、Ag、Au等元素丰度较高,是主要的矿源层。通过地质找矿工作的实践,笔者认为,该矿区是由火山喷流沉积-后期热液叠加富集的块状硫化物多金属矿床。

关 键 词:铅-锌矿床  矿床成因及找矿标志  地质特征  火山喷流沉积  银虎曼
文章编号:10000-5663(2007)04-0546-05
收稿时间:2007-03-25
修稿时间:2007年3月25日

Geological characteristics, metallogeny and prospecting indicators of the Pb-Zn deposit in Yinhuman
XIE Guo-min,YANG Shi-hui,XIE Ke.Geological characteristics, metallogeny and prospecting indicators of the Pb-Zn deposit in Yinhuman[J].Mineral Resources and Geology,2007,21(5):546-550.
Authors:XIE Guo-min  YANG Shi-hui  XIE Ke
Abstract:The Yinhuman lead-zinc deposit in its main ore-source stratum of the Huoshenmiao Formation in the Erlangping Group, where abundances of elements Pb.Zn.Ag.Au are highers is located in the east part of the Wangou polymetallic metallogenic zone. It is believed that the studying ore area is a polymetallic deposit of enriched massive sulfide resulted from the later hydrothermal superimposition on the volcanic cascade deposition.
Keywords:the Pb-Zn deposit  metallogeny and prospecting indicators  geological characteristics  volcanic cascade deposition  Yinhuman
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