2014•Contributions to Geology and Mineral Resources ResearchRequires access

Geological and geochemical characteristics of the Beizhihe Ag-Pb-Zn poly-metallic deposit in Beijing and its metallogenic model

Fang Tongmin

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Abstract

Beizhihe Ag-Pb-Zn deposit is located in the west mountainous area of Beijing.Ore bodies occur in Tieling and Wumishan formations of Jixian System and are controlled by fault and inter-formation fissure.Analysis of regional geology,ore-control structure,genesis and tempo-spatial evolution and geochemical characteristics of stream sediments and soil survey show that Ag-Pb-Zn anomaly is coincided with extension of ore bodies.Metallogenic model is built on basis of deposit and geochemical characteristics of the deposit.

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Beizhihe Ag-Pb-Zn deposit is located in the west mountainous area of Beijing.Ore bodies occur in Tieling and Wumishan formations of Jixian System and are controlled by fault and inter-formation fissure.Analysis of regional geology,ore-control structure,genesis and tempo-spatial evolution and geochemical characteristics of stream sediments and soil survey show that Ag-Pb-Zn anomaly is coincided with extension of ore bodies.Metallogenic model is built on basis of deposit and geochemical characteristics of the deposit.

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Available abstract

Beizhihe Ag-Pb-Zn deposit is located in the west mountainous area of Beijing.Ore bodies occur in Tieling and Wumishan formations of Jixian System and are controlled by fault and inter-formation fissure.Analysis of regional geology,ore-control structure,genesis and tempo-spatial evolution and geochemical characteristics of stream sediments and soil survey show that Ag-Pb-Zn anomaly is coincided with extension of ore bodies.Metallogenic model is built on basis of deposit and geochemical characteristics of the deposit.

Key concepts: Geology, Geochemistry, Beijing, Fault (geology), Mining engineering, China, Seismology, Archaeology

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