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    中国百强科技报刊

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    Volume 45 Issue 12
    Dec.  2020
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    Lü Xinbiao, Yang Junsheng, Fan Xiejun, Wei Wei, Mei Wei, Ruan Banxiao, Wang Xiangdong, Gun Minshan, 2020. Geology and Genesis of Lead-Zinc Polymetallic Deposits in the Great Xing'an Range. Earth Science, 45(12): 4399-4427. doi: 10.3799/dqkx.2020.995
    Citation: Lü Xinbiao, Yang Junsheng, Fan Xiejun, Wei Wei, Mei Wei, Ruan Banxiao, Wang Xiangdong, Gun Minshan, 2020. Geology and Genesis of Lead-Zinc Polymetallic Deposits in the Great Xing'an Range. Earth Science, 45(12): 4399-4427. doi: 10.3799/dqkx.2020.995

    Geology and Genesis of Lead-Zinc Polymetallic Deposits in the Great Xing'an Range

    doi: 10.3799/dqkx.2020.995
    • Received Date: 2020-11-01
    • Publish Date: 2020-12-15
    • As breakthrough achieved in recent exploration,lead-zinc polymetallic deposits in the Great Xing'an Range have shown complexity and differences in aspects of mineralized elements,temporal-spatial distribution,genesis and so on. For a further inspection of the variation and its internal causes,data from medium-large sized deposits are compiled and compared in this study. Main conclusions are summarized: (1) these deposits formed three parallel NE trending belts with a higher intensity in the southern belt; (2) two major phases of mineralization are recognized as in the Middle-Late Triassic (less important) and the predominant Late Jurassic-Early Cretaceous,superimposed mineralization is also notable; (3) epithermal deposit is representative in the northern belt,while skarn- and magmatic hydrothermal vein-types are more common in the middle and the southern belts; (4) under the Late Jurassic-Early Cretaceous extensional environment,enormous acidic-intermediate magma emplacement affected the whole Great Xing'an Range,leading to the formation of various lead-zinc polymetallic deposits,among which tin-rich ones in the southern belt exhibit genetic links to highly differentiated magma; (5) strong spatial association between the fluorine-,manganese-related alteration and mineralization is noticed; (6) deposits in the northern,middle and southern belts have their sulfur sourced from genetically related volcanic-subvolcanic rocks,ore-related magma and a combination of magma and country rocks; (7) Pb isotope data indicate that most deposits have a mixed lead source from orogeny,probably due to similar regional post-orogenic background in the Late Jurassic-Early Cretaceous; (8) as suggested by H-O isotopic data,meteoric water contributes more for fluid source in epithermal deposits,despite a more crucial role of magmatic water in skarn- and magmatic hydrothermal vein-type deposits.

       

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