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    如何有效厘定增生造山作用时限?

    肖文交 宋东方 毛启贵 万博 张继恩 敖松坚 张志勇

    肖文交, 宋东方, 毛启贵, 万博, 张继恩, 敖松坚, 张志勇, 2022. 如何有效厘定增生造山作用时限?. 地球科学, 47(10): 3770-3771. doi: 10.3799/dqkx.2022.802
    引用本文: 肖文交, 宋东方, 毛启贵, 万博, 张继恩, 敖松坚, 张志勇, 2022. 如何有效厘定增生造山作用时限?. 地球科学, 47(10): 3770-3771. doi: 10.3799/dqkx.2022.802
    Xiao Wenjiao, Song Dongfang, Mao Qigui, Wan Bo, Zhang Ji’en, Ao Songjian, Zhang Zhiyong, 2022. How to Determine the Time Limits of Accretionary Orogenesis?. Earth Science, 47(10): 3770-3771. doi: 10.3799/dqkx.2022.802
    Citation: Xiao Wenjiao, Song Dongfang, Mao Qigui, Wan Bo, Zhang Ji’en, Ao Songjian, Zhang Zhiyong, 2022. How to Determine the Time Limits of Accretionary Orogenesis?. Earth Science, 47(10): 3770-3771. doi: 10.3799/dqkx.2022.802

    如何有效厘定增生造山作用时限?

    doi: 10.3799/dqkx.2022.802
    基金项目: 

    国家自然科学基金项目 41888101

    国家自然科学基金项目 41730210

    国家重点研发计划项目 2017YFC0601206

    详细信息
      作者简介:

      肖文交(1967-),男,研究员,博士生导师,中国科学院院士,欧洲科学院外籍院士,主要从事沉积大地构造学、造山带构造过程与成矿作用等研究.E-mail:wj-xiao@mail.iggcas.ac.cn

    How to Determine the Time Limits of Accretionary Orogenesis?

    • [1] Decou, A., von Eynatten, H., Mamani, M., et al., 2011. Cenozoic Forearc Basin Sediments in Southern Peru (15-18°S): Stratigraphic and Heavy Mineral Constraints for Eocene to Miocene Evolution of the Central Andes. Sedimentary Geology, 237(1): 55-72.
      [2] Hall, R., 2009. The Eurasian SE Asian Margin as a Modern Example of an Accretionary Orogen. Geological Society, London, Special Publications, 318(1): 351-372. doi: 10.1144/SP318.13
      [3] Şengör, A. M. C., Natal'in, B. A., Burtman, V. S., 1993. Evolution of the Altaid Tectonic Collage and Palaeozoic Crustal Growth in Eurasia. Nature, 364(6435): 299-307. https://doi.org/10.1038/364299a0
      [4] Song, D. F., Xiao, W. J., Collins, A. S., et al., 2018. Final Subduction Processes of the Paleo-Asian Ocean in the Alxa Tectonic Belt (NW China): Constraints from Field and Chronological Data of Permian Arc-Related Volcano-Sedimentary Rocks. Tectonics, 37(2/3): 1658-1687. https://doi.org/10.1029/2017tc004919
      [5] Song, D. F., Xiao, W. J., Windley, B. F., et al., 2021. Closure of the Paleo-Asian Ocean in the Middle-Late Triassic (Ladinian-Carnian): Evidence from Provenance Analysis of Retroarc Sediments. Geophysical Research Letters, 48(14): e2021GL094276. https://doi.org/10.1029/2021gl094276
      [6] Turnbull, R., Tulloch, A., Ramezani, J., et al., 2016. Extension-Facilitated Pulsed S-I-A-Type "Flare-up" Magmatism at 370 Ma along the Southeast Gondwana Margin in New Zealand: Insights from U-Pb Geochronology and Geochemistry. Geological Society of America Bulletin, 128(9/10): 1500-1520.
      [7] Xiao, W. J., Windley, B. F., Sun, S., et al., 2015. A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion. Annual Review of Earth and Planetary Sciences, 43(1): 477-507. https://doi.org/10.1146/annurev-earth-060614-105254
      [8] Zapata, S., Cardona, A., Jaramillo, J., et al., 2019. Cretaceous Extensional and Compressional Tectonics in the Northwestern Andes, Prior to the Collision with the Caribbean Oceanic Plateau. Gondwana Research, 66: 207-226. doi: 10.1016/j.gr.2018.10.008
      [9] 李继亮, 2004. 增生型造山带的基本特征. 地质通报, 23(9): 947-951. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2004Z2017.htm
      [10] 肖文交, 李继亮, 宋东方, 等, 2019. 增生型造山带结构解析与时空制约. 地球科学, 44(5): 1661-1687. doi: 10.3799/dqkx.2019.979
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    出版历程
    • 刊出日期:  2022-10-25

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