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    秦岭隆升过程及其如何控制气候环境?

    董云鹏 杨钊 孙圣思 史小辉 何登峰 惠博 龙晓平 郭安林

    董云鹏, 杨钊, 孙圣思, 史小辉, 何登峰, 惠博, 龙晓平, 郭安林, 2022. 秦岭隆升过程及其如何控制气候环境?. 地球科学, 47(10): 3834-3836. doi: 10.3799/dqkx.2022.830
    引用本文: 董云鹏, 杨钊, 孙圣思, 史小辉, 何登峰, 惠博, 龙晓平, 郭安林, 2022. 秦岭隆升过程及其如何控制气候环境?. 地球科学, 47(10): 3834-3836. doi: 10.3799/dqkx.2022.830
    Dong Yunpeng, Yang Zhao, Sun Shengsi, Shi Xiaohui, He Dengfeng, Hui Bo, Long Xiaoping, Guo Anlin, 2022. Uplifting Process of the Qinling Mountains and How to Control the Climate and Environment Change?. Earth Science, 47(10): 3834-3836. doi: 10.3799/dqkx.2022.830
    Citation: Dong Yunpeng, Yang Zhao, Sun Shengsi, Shi Xiaohui, He Dengfeng, Hui Bo, Long Xiaoping, Guo Anlin, 2022. Uplifting Process of the Qinling Mountains and How to Control the Climate and Environment Change?. Earth Science, 47(10): 3834-3836. doi: 10.3799/dqkx.2022.830

    秦岭隆升过程及其如何控制气候环境?

    doi: 10.3799/dqkx.2022.830
    详细信息
      作者简介:

      董云鹏(1967—),男,博士,教授,长期从事大地构造学与地球系统科学研究.E-mail:dongyp@nwu.edu.cn

    Uplifting Process of the Qinling Mountains and How to Control the Climate and Environment Change?

    • [1] Dong, Y. P., Neubauer, F., Genser, J., et al., 2018. Timing of Orogenic Exhumation Processes of the Qinling Orogen: Evidence from 40 Ar/39 Ar Dating. Tectonics, 37(10): 4037-4067. https://doi.org/10.1029/2017tc004765
      [2] Dong, Y. P., Sun, S. S., Santosh, M., et al., 2021. Central China Orogenic Belt and Amalgamation of East Asian Continents. Gondwana Research, 100: 131-194. https://doi.org/10.1016/j.gr.2021.03.006
      [3] Dong, Y. P., Sun, S. S., Santosh, M., et al., 2022a. Cross Orogenic Belts in Central China: Implications for the Tectonic and Paleogeographic Evolution of the East Asian Continental Collage. Gondwana Research, 109: 18-88. https://doi.org/10.1016/j.gr.2022.04.012
      [4] Dong, Y. P., Shi, X. H., Sun, S. S., et al., 2022b. Co-Evolution of the Cenozoic Tectonics, Geomorphology, Environment and Ecosystem in the Qinling Mountains and Adjacent Areas, Central China. Geosystems and Geoenvironment, 1(2): 100032. https://doi.org/10.1016/j.geogeo.2022.100032
      [5] Shi, X. H., Yang, Z., Dong, Y. P., et al., 2018. Longitudinal Profile of the Upper Weihe River: Evidence for the Late Cenozoic Uplift of the Northeastern Tibetan Plateau. Geological Journal, 53: 364-378. https://doi.org/10.1002/gj.3195
      [6] Shi, X. H., Yang, Z., Dong, Y. P., et al., 2020. Geomorphic Indices and Longitudinal Profile of the Daba Shan, Northeastern Sichuan Basin: Evidence for the Late Cenozoic Eastward Growth of the Tibetan Plateau. Geomorphology, 353: 107031. https://doi.org/10.1016/j.geomorph.2020.107031
      [7] Yang, Z., Shen, C. B., Ratschbacher, L., et al., 2017. Sichuan Basin and Beyond: Eastward Foreland Growth of the Tibetan Plateau from an Integration of Late Cretaceous-Cenozoic Fission Track and (U-Th)/He Ages of the Eastern Tibetan Plateau, Qinling, and Daba Shan. Journal of Geophysical Research: Solid Earth, 122(6): 4712-4740. https://doi.org/10.1002/2016jb013751
      [8] 董云鹏, 任建国, 张志飞, 等, 2022. 地质学科未来5~10年发展战略: 趋势与对策. 科学通报, 67(23): 2708-2718. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB202223004.htm
      [9] 张国伟, 郭安林, 董云鹏, 等, 2019. 关于秦岭造山带. 地质力学学报, 25(5): 746-768. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLX201905009.htm
      [10] 张国伟, 张本仁, 袁学诚, 等, 2001. 秦岭造山带与大陆动力学. 北京, 科学出版社.
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    • 刊出日期:  2022-10-25

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