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ZHOUYong-Zhang, YANGWei, YUPeng-Peng, ZHENGYi, SHENWen-Jie, ZHANGQian-Long. 2022. Considerations on Study of Paleo-oceanic Seafloor Rexhalative Hydrothermal Sedimentation and Related Mineral Deposits of the Qinzhou-Hangzhou Metallogenic Belt, South China. South China Geology, 38(3): 382-393. doi: 10.3969/j.issn.2097-0013.2022.03.002
Citation: ZHOUYong-Zhang, YANGWei, YUPeng-Peng, ZHENGYi, SHENWen-Jie, ZHANGQian-Long. 2022. Considerations on Study of Paleo-oceanic Seafloor Rexhalative Hydrothermal Sedimentation and Related Mineral Deposits of the Qinzhou-Hangzhou Metallogenic Belt, South China. South China Geology, 38(3): 382-393. doi: 10.3969/j.issn.2097-0013.2022.03.002
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Considerations on Study of Paleo-oceanic Seafloor Rexhalative Hydrothermal Sedimentation and Related Mineral Deposits of the Qinzhou-Hangzhou Metallogenic Belt, South China

  • 1. Center for Earth Environment & Resources, Sun Yat-sen University, Guangzhou 510275, Guangdong, China

  • 2.Guangdong Provinical Key Laboratory of Mineral Resources and Geological Processes, Guangzhou 510275, Guangdong, China

  • 3. Department of Earth Sciences, Sun Yat-sen University, Guangzhou 510275, Guangdong, China

  • 4. Guangdong Institute of Quanlity Resource & Environment, Guangzhou 510000, Guangdong, China

Received Date:  11 April 2022
Revised Date:  05 August 2022
    Abstract
  • The Qinzhou-Hangzhou Metallogenic Belt (QHMB) is a giant tectonic junction zone between the Yangtze and Cathaysia palaeo-continents. The multi-layered distribution of ancient marine submarine sedimentary exhalative (Sedex) makes it an ideal place to study the precise spatial and temporal structure of the Sedex system and the coupling mechanism of the evolution of the palaeo-continental tectonic junction belt. Based on the review of existing studies, this paper proposes more intensive research on the palaeo-oceanic Sedex and its mineralisation in the QHMB. From the perspective that the QHMB is also the junction belt of two palaeo-terrestrial zones, we analyse the spatial and temporal distribution characteristics and development setting of the Sedex deposits, so to distinguish different types of sedimentary construction, dissect the geochemical three-dimensional spatial structure of the Sedex system, and reveal the coupling mechanism between the spatial and temporal structure of the Sedex system and the evolution of the palaeo-terrestrial tectonic junction zone. With new equipment, new tools and new ideas, the homogeneity and diversity of mineralogy, petrology and geochemistry of different layers and types of the Sedex ore deposits could be identified, and the precise differences in the microstructure and micro-composition of different Sedex ore minerals and the isotopic information of B, S, Fe, Cu and Zn have been analysed to reveal these homogeneity, diversity and precise differences in correspondence with the inter-continent tectonic system and the evolution of the Sedex system. The results would deepen the understanding of the mineralisation of the Sedex system, provide guidance for the exploration of submarine Sedex deposits and improve the mineralisation theory research of the QHMB.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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