深俯冲地壳物质如何循环至地表？-Reference-Cited by-同舟云学术

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深俯冲地壳物质如何循环至地表？

Published:2022 Issue:10 Volume:47 Page:3772
ISSN:1000-2383
Container-title:Earth Science-Journal of China University of Geosciences
language:
Short-container-title:Eart. Scie.

Author:

Wu Weiwei,Yang Jingsui

Publisher

Editorial Office of Earth Science

Subject

General Earth and Planetary Sciences,Computer Science Applications,Building and Construction

Reference45 articles.

1. Arai, S., 2013. Conversion of Low-Pressure Chromitites to Ultrahigh-Pressure Chromitites by Deep Recycling: A Good Inference. Earth and Planetary Science Letters, 379: 81-87. https://doi.org/10.1016/j.epsl.2013.08.006

2. Arai, S., Miura, M., 2016. Formation and Modification of Chromitites in the Mantle. Lithos, 264: 277-295. https://doi.org/10.1016/j.lithos.2016.08.039

3. Butler, J. P., Beaumont, C., 2017. Subduction Zone Decoupling/Retreat Modeling Explains South Tibet (Xigaze) and other Supra-Subduction Zone Ophiolites and Their UHP Mineral Phases. Earth and Planetary Science Letters, 463: 101-117. https://doi.org/10.1016/j.epsl.2017.01.025

4. Chen, L. H., Wang, X. J., Liu, S. G., 2022. Probing Recycled Carbonate in the Lower Mantle. National Science Review, 9(6): nwac061. https://doi.org/10.1093/nsr/nwac061

5. Courtillot, V., Olson, P., 2007. Mantle Plumes Link Magnetic Superchrons to Phanerozoic Mass Depletion Events. Earth and Planetary Science Letters, 260(3/4): 495-504. https://doi.org/10.1016/j.epsl.2007.06.003

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