Dual origin of ferropericlase inclusions within super-deep diamonds

Ferropericlase [(Mg,Fe)O] is one of the major constituents of Earth's lower mantle and the most abundant mineral inclusion in sub-lithospheric diamonds. Although a lower mantle origin for ferropericlase inclusions has often been suggested, some studies have proposed that many of these inclusion...

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Veröffentlicht in:	Earth and planetary science letters 2023-04, Vol.608 (C), p.118081, Article 118081
Hauptverfasser:	Lorenzon, Sofia, Wenz, Michelle, Nimis, Paolo, Jacobsen, Steven D., Pasqualetto, Leonardo, Pamato, Martha G., Novella, Davide, Zhang, Dongzhou, Anzolini, Chiara, Regier, Margo, Stachel, Thomas, Pearson, D. Graham, Harris, Jeffrey W., Nestola, Fabrizio
Format:	Artikel
Sprache:	eng
Schlagworte:	crystallographic orientation relationship diamond ferropericlase Geochemistry & Geophysics GEOSCIENCES growth relationship protogenesis syngenesis
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