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    中国百强科技报刊

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    Liu Kunfeng, Wang Yonghe, Jiang Gaolei, Zhang Simin, Zhang kexin, 2014. Evolution of Neoproterozoic-Mesozoic Sedimentary Basins of West Kunlun Area. Earth Science, 39(8): 987-999. doi: 10.3799/dqkx.2014.090
    Citation: Liu Kunfeng, Wang Yonghe, Jiang Gaolei, Zhang Simin, Zhang kexin, 2014. Evolution of Neoproterozoic-Mesozoic Sedimentary Basins of West Kunlun Area. Earth Science, 39(8): 987-999. doi: 10.3799/dqkx.2014.090

    Evolution of Neoproterozoic-Mesozoic Sedimentary Basins of West Kunlun Area

    doi: 10.3799/dqkx.2014.090
    • Received Date: 2014-03-12
    • Publish Date: 2014-08-01
    • West Kunlun orogenic belt is located in the northwest margin of the Qinghai-Tibet Plateau, and in the southwest edge of Tarim basin. This belt is an important part of the central orogenic belt. It has experienced a long and complicated tectonic-sedimentary evolution. This paper presents lithostratigraphy of outcrops in five stratigraphic subregions and their corresponding sedimentary basin types in West Kunlun orogenic belt. The evolutionary history of sedimentary basins in West Kunlun is explored and divided into following three stages from Neoproterozoic to Mesozoic in this study: (1) the stage of continental break-up and the formation of oceanic crust in Neoproterozoic; (2) the stage of plate mechanism evolution in Early Paleozoic-Middle Triassic; (3) the stage of evolution in intracontinental since Late Triassic.

       

    • 致谢: 本文撰写过程中得到了西北各省地质调查院、中国地质调查局发展研究中心、西安地质调查中心、成都地质调查中心、全国重要矿产成矿背景项目组的所有专家学者们的帮助,提供了大量基础资料,对本文的形成起到了奠基和指导作用,在此谨表谢意.西安地质矿产研究所冯益民研究员对论文的修改提出宝贵建议;在论文的撰写程中, 徐增连博士、孔令耀硕士、杨翠英女士提供了帮助, 在此一并表示衷心感谢!
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