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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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Bibliographic Details
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, Vincenzo^1,2 (AUTHOR) vincenzo.stagno@uniroma1.it, Bindi, Luca³ (AUTHOR), Bonechi, Barbara⁴ (AUTHOR), Greaux, Steeve^5,6 (AUTHOR), Aulbach, Sonja⁷ (AUTHOR), Irifune, Tetsuo^5,6 (AUTHOR), Lupi, Stefano^8,9 (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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