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Cubic Fe-bearing majorite synthesized at 18–25 GPa and 1000 °C: implications for element transport, subducted slab rheology and diamond formation.

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Title: Cubic Fe-bearing majorite synthesized at 18–25 GPa and 1000 °C: implications for element transport, subducted slab rheology and diamond formation.
Authors: Stagno, Vincenzo1,2 (AUTHOR) vincenzo.stagno@uniroma1.it, Bindi, Luca3 (AUTHOR), Bonechi, Barbara4 (AUTHOR), Greaux, Steeve5,6 (AUTHOR), Aulbach, Sonja7 (AUTHOR), Irifune, Tetsuo5,6 (AUTHOR), Lupi, Stefano8,9 (AUTHOR), Marras, Giulia1 (AUTHOR), McCammon, Catherine A.10 (AUTHOR), Nazzari, Manuela2 (AUTHOR), Piccirilli, Federica9 (AUTHOR), Poe, Brent11 (AUTHOR), Romano, Claudia12 (AUTHOR), Scarlato, Piergiorgio2 (AUTHOR)
Source: Scientific Reports. 11/18/2023, Vol. 13 Issue 1, p1-12. 12p.
Database: Academic Search Ultimate
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ISSN:20452322
DOI:10.1038/s41598-023-43037-6