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Major types and time–space distribution of Mesozoic ore deposits in South China and their geodynamic settings
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  • 作者：Mao Jingwen (1)
    Cheng Yanbo (2)
    Chen Maohong (1) (2)
    Franco Pirajno (1) (3)
  • 关键词：Granite ; related polymetallic Sn–W ; Porphyry Cu–Mo-Au) ; Epithermal Cu–Au–Ag ; South China
  • 刊名：Mineralium Deposita
  • 出版年：2013
  • 出版时间：March 2013
  • 年：2013
  • 卷：48
  • 期：3
  • 页码：267-294
  • 全文大小：1917KB
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  • 作者单位：Mao Jingwen (1)
    Cheng Yanbo (2)
    Chen Maohong (1) (2)
    Franco Pirajno (1) (3)

    1. MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037, China
    2. Faculty of Earth Sciences and Resources, China University of Geosciences, Beijing, 100083, China
    3. Centre for Exploration Targeting, University of Western Australia, 35 Stirling Highway, Crawley, WA, 6008, Australia
  • ISSN：1432-1866
文摘
The ore deposits of the Mesozoic age in South China can be divided into three groups, each with different metal associations and spatial distributions and each related to major magmatic events. The first event occurred in the Late Triassic (230-10?Ma), the second in the Mid–Late Jurassic (170-50?Ma), and the third in the Early–Mid Cretaceous (120-0?Ma). The Late Triassic magmatic event and associated mineralization is characterized by peraluminous granite-related W–Sn–Nb–Ta mineral deposits. The Triassic ore deposits are considerably disturbed or overprinted by the later Jurassic and Cretaceous tectono-thermal episodes. The Mid–Late Jurassic magmatic and mineralization events consist of 170-60?Ma porphyry–skarn Cu and Pb–Zn–Ag vein deposits associated with I-type granites and 160-50?Ma metaluminous granite-related polymetallic W–Sn deposits. The Late Jurassic metaluminous granite-related W–Sn deposits occur in a NE-trending cluster in the interior of South China, such as in the Nanling area. In the Early–Mid Cretaceous, from about 120 to 80?Ma, but peaking at 100-0?Ma, subvolcanic-related Fe deposits developed and I-type calc-alkaline granitic intrusions formed porphyry Cu–Mo and porphyry-epithermal Cu–Au–Ag mineral systems, whereas S-type peraluminous and/or metaluminous granitic intrusions formed polymetallic Sn deposits. These Cretaceous mineral deposits cluster in distinct areas and are controlled by pull-apart basins along the South China continental margin. Based on mineral assemblage, age, and space–time distribution of these mineral systems, integrated with regional geological data and field observations, we suggest that the three magmatic–mineralization episodes are the result of distinct geodynamic regimes. The Triassic peraluminous granites and associated W–Sn–Nb–Ta mineralization formed during post-collisional processes involving the South China Block, the North China Craton, and the Indo-China Block, mostly along the Dabie-Sulu and Songma sutures. Jurassic events were initially related to the shallow oblique subduction of the Izanagi plate beneath the Eurasian continent at about 175?Ma, but I-type granitoids with porphyry Cu and vein-type Pb–Zn–Ag deposits only began to form as a result of the breakup of the subducted plate at 170-60?Ma, along the NNE-trending Qinzhou-Hangzhou belt (also referred to as Qin-Hang or Shi-Hang belt), which is the Neoproterozoic suture that amalgamates the Yangtze Craton and Cathaysia Block. A large subduction slab window is assumed to have formed in the Nanling and adjacent areas in the interior of South China, triggering the uprise of asthenospheric mantle into the upper crust and leading to the emplacement of metaluminous granitic magma and associated polymetallic W–Sn mineralization. A relatively tectonically quiet period followed between 150 and 135?Ma in South China. From 135?Ma onward, the angle of convergence of the Izanagi plate changed from oblique to parallel to the coastline, resulting in continental extensional tectonics and reactivation of regional-scale NE-trending faults, such as the Tan-Lu fault. This widespread extension also promoted the development of NE-trending pull-apart basins and metamorphic core complexes, accompanied by volcanism and the formation of epithermal Cu–Au deposits, granite-related polymetallic Sn-W) deposits and hydrothermal U deposits between 120 and 80?Ma (with a peak activity at 100-0?Ma).

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