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    Volume 49 Issue 6
    Jun.  2024
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    Article Navigation >  Earth Science  > 2024  >  49(6): 2001-2023
    Tao Lirong, Cao Shuyun, Li Wenyuan, Cheng Xuemei, Wang Haobo, Dong Yanlong, 2024. Evolution Characteristics and Rheological Significance of Dehydration Melting and Water-Fluxed Melting in Deep Continental Crust. Earth Science, 49(6): 2001-2023. doi: 10.3799/dqkx.2024.007
    Citation: Tao Lirong, Cao Shuyun, Li Wenyuan, Cheng Xuemei, Wang Haobo, Dong Yanlong, 2024. Evolution Characteristics and Rheological Significance of Dehydration Melting and Water-Fluxed Melting in Deep Continental Crust. Earth Science, 49(6): 2001-2023. doi: 10.3799/dqkx.2024.007
    shu

    Evolution Characteristics and Rheological Significance of Dehydration Melting and Water-Fluxed Melting in Deep Continental Crust

    doi: 10.3799/dqkx.2024.007

    • School of Earth Sciences, State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

    • Received Date: 2023-11-09
      Available Online: 2024-07-11
    • Publish Date: 2024-06-25
      Abstract
    • Anatexis is significant for the evolution and rheological properties of the continental crust, linking metamorphism, tectonic deformation, and magmatic activities in deep crust. According to the presence or absence of free water, anatexis can be divided into water-fluxed melting and dehydration melting. Dehydration melting involves the breakdown of hydrous phases, such as muscovite, biotite or amphibole. Generally, dehydration melting reactions begin at ~650 ℃ and produce melt, peritectic garnet and K-feldspar. Melt resulting from dehydration melting is water unsaturated, characterized by high Rb, high Rb/Sr ratio, high 87Sr/86Sr ratio, and low Sr, Ba, Ca. Melt productivity of dehydration melting reaction is controlled by P-T condition and water content in rock, and it is only possible to produce a large amount of melt at granulite facies. Water-fluxed melting reactions involve the presence of free water. Its most significant feature is that the temperature required is relatively low, and can produce voluminous melting at amphibolite facies. The resulting melt is water-saturated or water unsaturated that can extract from the source. Melt derived from water-fluxed melting reactions has high Sr, Ba, Ca, low Rb/Sr ratio and low Rb. Anatexis has a profound impact on the thermodynamic and rheological properties of the rocks. At the same time, the movement of melt out of the lower continental crust promotes the chemical differentiation of the crust and forms a wide range of leucogranite, playing a crucial role in the origin, reworking, and stability of the continental crust.

       

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