Melting of Garnet Peridotite and the Origin of Komatiite and Depleted Lithosphere

DOI DOI PDF 被引用文献53件 オープンアクセス

書誌事項

公開日
1998-01-01
DOI
  • 10.1093/petroj/39.1.29
  • 10.1093/petrology/39.1.29
公開者
Oxford University Press (OUP)

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説明

However, it can be a residue of komatiite melt extraction at >7 Melting experiments on fertile peridotite KR4003, a ‘pyrolitic’ GPa from a mantle enriched in SiO2 relative to pyrolite. composition, were made from 3 to 7 GPa in piston-cylinder and multi-anvil apparatus. Temperature gradients across the sample were minimized (<25°C), and the compositions of all phases were determined. Modal abundances of coexisting phases were calculated by mass balance, and the results were used to determine phase

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