Carbonated Big Mantle Wedge Extending to the NE Edge of the Stagnant Pacific Slab: Constraints from Late Mesozoic-Cenozoic Basalts from Far Eastern Russia
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12583-021-1516-x.pdf
Reference89 articles.
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3. Cai, R. H., Liu, J. G., Pearson, D. G., et al., 2021. Oxidation of the Deep Big Mantle Wedge by Recycled Carbonates: Constraints from Highly Siderophile Elements and Osmium Isotopes. Geochimica et Cosmochimica Acta, 295: 207–223. https://doi.org/10.1016/j.gca.2020.12.019
4. Chen, H., Savage, P. S., Teng, F. Z., et al., 2013. Zinc Isotope Fractionation during Magmatic Differentiation and the Isotopic Composition of the Bulk Earth. Earth and Planetary Science Letters, 369/370: 34–42. https://doi.org/10.1016/j.epsl.2013.02.037
5. Chen, S. S., Liu, J. Q., Chen, S. S., et al., 2015. Variations in the Geochemical Structure of the Mantle Wedge beneath the Northeast Asian Marginal Region from Pre- to Post-Opening of the Japan Sea. Lithos, 224/225: 324–341. https://doi.org/10.1016/j.lithos.2015.03.008
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