H2O-induced sedimentary carbon migration from subducting slabs to the forearc mantle
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s11430-022-9965-5.pdf
Reference55 articles.
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3. Amsellem E, Moynier F, Bertrand H, Bouyon A, Mata J, Tappe S, Day J M D. 2020. Calcium isotopic evidence for the mantle sources of carbonatites. Sci Adv, 6: eaba3269
4. Barry P H, de Moor J M, Giovannelli D, Schrenk M, Hummer D R, Lopez T, Pratt C A, Segura Y A, Battaglia A, Beaudry P, Bini G, Cascante M, d’Errico G, di Carlo M, Fattorini D, Fullerton K, Gazel E, González G, Halldórsson S A, Iacovino K, Ilanko T, Kulongoski J T, Manini E, Martínez M, Miller H, Nakagawa M, Ono S, Patwardhan S, Ramírez C J, Regoli F, Smedile F, Turner S, Vetriani C, Yücel M, Ballentine C J, Fischer T P, Hilton D R, Lloyd K G. 2019. Forearc carbon sink reduces long-term volatile recycling into the mantle. Nature, 568: 487–492
5. Bebout G E. 2007. Metamorphic chemical geodynamics of subduction zones. Earth Planet Sci Lett, 260: 373–393
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