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    岩浆如何链接地球深部过程与浅部系统?

    郑建平 马强 苏玉平 陈明 平先权 戴宏坤

    郑建平, 马强, 苏玉平, 陈明, 平先权, 戴宏坤, 2022. 岩浆如何链接地球深部过程与浅部系统?. 地球科学, 47(10): 3779-3780. doi: 10.3799/dqkx.2022.805
    引用本文: 郑建平, 马强, 苏玉平, 陈明, 平先权, 戴宏坤, 2022. 岩浆如何链接地球深部过程与浅部系统?. 地球科学, 47(10): 3779-3780. doi: 10.3799/dqkx.2022.805
    Zheng Jianping, Ma Qiang, Su Yuping, Chen Ming, Ping Xianquan, Dai Hongkun, 2022. How does the Magma Link the Earth Deep Process with the Shallow System?. Earth Science, 47(10): 3779-3780. doi: 10.3799/dqkx.2022.805
    Citation: Zheng Jianping, Ma Qiang, Su Yuping, Chen Ming, Ping Xianquan, Dai Hongkun, 2022. How does the Magma Link the Earth Deep Process with the Shallow System?. Earth Science, 47(10): 3779-3780. doi: 10.3799/dqkx.2022.805

    岩浆如何链接地球深部过程与浅部系统?

    doi: 10.3799/dqkx.2022.805
    详细信息
      作者简介:

      郑建平(1964-), 男,教授,主要研究深源岩石与岩石圈演化.E-mail: jpzheng@cug.edu.cn

    How does the Magma Link the Earth Deep Process with the Shallow System?

    • [1] Aiuppa, A., Casetta, F., Coltorti, M., et al., 2021. Carbon Concentration Increases with Depth of Melting in Earth's Upper Mantle. Nature Geoscience, 14(9): 697-703. https://doi.org/10.1038/s41561-021-00797-y
      [2] Arzilli, F., Polacci, M., LaSpina, G., et al., 2022. Dendritic Crystallization in Hydrous Basaltic Magmas Controls Magma Mobility within the Earth's Crust. Nature Communications, 13(1): 3354. https://doi.org/10.1038/s41467-022-30890-8
      [3] Cashman, K. V., Sparks, R. S. J., Blundy, J. D., 2017. Vertically Extensive and Unstable Magmatic Systems: A Unified View of Igneous Processes. Science, 355(6331): eaag3055. https://doi.org/10.1126/science.aag3055
      [4] Coleman, D. S., Mills, R. D., Zimmerer, M. J., 2016. The Pace of Plutonism. Elements, 12(2): 97-102. https://doi.org/10.2113/gselements.12.2.97
      [5] Hofmann, A. W., 2014. Sampling Mantle Heterogeneity through Oceanic Basalts: Isotopes and Trace Elements. In: Holland, H. D., Turekian, K. K., eds., Treatise on Geochemistry (Second Edition). Oxford: Elsevier, 67-101.
      [6] Langmuir, C. H., Broecker, W. S, 2012. How to Build a Habitable Planet: The Story of Earth from the Big Bang to Humankind. Princeton University Press, Princeton and Oxford.
      [7] Lee, C. T. A., Yeung, L. Y., McKenzie, N. R., et al., 2016. Two-Step Rise of Atmospheric Oxygen Linked to the Growth of Continents. Nature Geoscience, 9(6): 417-424. https://doi.org/10.1038/ngeo2707
      [8] Ma, Q., Zheng, J. P., Xu, Y. G., et al., 2015. Are Continental "Adakites"Derived from Thickened or Foundered Lower Crust? Earth and Planetary Science Letters, 419: 125-133. https://doi.org/10.1016/j.epsl.2015.02.036
      [9] Sun, H., Xiao, Y. L., Gao, Y. J., et al., 2018. Rapid Enhancement of Chemical Weathering Recorded by Extremely Light Seawater Lithium Isotopes at the Permian-Triassic Boundary. Proceedings of the National Academy of Sciences of the United States of America, 115(15): 3782-3787. https://doi.org/10.1073/pnas.1711862115
      [10] Zheng, J. P., Griffin, W. L., O'Reilly, S. Y., et al., 2008. Continental Collision and AccretionRecorded in the Deep Lithosphere of Central China. Earth and Planetary Science Letters, 269(3-4): 497-507. https://doi.org/10.1016/j.epsl.2008.03.003
      [11] Zheng, J. P., Lee, C. T. A., Lu, J. G., etal., 2015. Refertilization-Driven Destabilization of Subcontinental Mantle and the Importance of Initial Lithospheric Thickness for the Fate of Continents. Earth and Planetary Science Letters, 409: 225-231. https://doi.org/10.1016/j.epsl.2014.10.042
      [12] Zindler, A., Hart, S., 1986. Chemical Geodynamics. Annual Review of Earth and Planetary Sciences, 14: 493-571. https://doi.org/10.1146/annurev.ea.14.050186.002425
      [13] 郑建平, 戴宏坤, 2018. 西太平洋板片俯冲与后撤引起华北东部地幔置换并导致陆内盆-山耦合. 中国科学: 地球科学, 48(4): 436-456. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201804004.htm
      [14] 郑建平, 夏冰, 戴宏坤, 等, 2021. 地球物理观察和岩石包体约束华北岩石圈地幔结构、性质及过程. 中国科学: 地球科学, 51(2): 201-217. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK202102003.htm
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    • 刊出日期:  2022-10-25

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