Melting of enstatite (MgSiO 3 ) from 10 to 16.5 GPa and the forsterite (Mg 2 SiO 4 )-majorite (MgSiO 3 ) eutectic at 16.5 GPa: Implications for the origin of the mantle

✍ Scribed by Presnall, D. C.; Gasparik, T.

• Book ID: 118671953
• Publisher: American Geophysical Union
• Year: 1990
• Tongue: English
• Weight: 921 KB
• Volume: 95
• Category: Article
• ISSN: 0148-0227
• DOI: 10.1029/jb095ib10p15771