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- W2076623296 abstract "[1] A suite of garnet-bearing xenoliths that is dominantly composed of olivine, clinopyroxene, and garnet, from Oahu, Hawaii is discussed. All the minerals are in Mg# equilibrium with each other. High Fe/Mg of constituent minerals, high TiO2, Al2O3, Na2O of cpx, and low Cr-garnet preclude these xenoliths from being residues of partial melting. Combined petrography, mineral chemistry, and high-pressure liquidus phase equilibria indicate that these xenoliths are high pressure cumulates and originated as products of magma fractionation at a depth of >100 km, corresponding to the uppermost part of the asthenosphere. These depth constraints are about 15 km more than the seismically detected lithosphere-asthenosphere boundary. It is proposed here that the top of the asthenosphere beneath Oahu, Hawaii is a network of magma chambers where considerable amount of magma ponding and subsequent fractionation takes place." @default.
- W2076623296 created "2016-06-24" @default.
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- W2076623296 date "2004-01-01" @default.
- W2076623296 modified "2023-10-01" @default.
- W2076623296 title "The depth of magma fractionation in the oceanic mantle: Insights from garnet- bearing xenoliths from Oahu, Hawaii" @default.
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- W2076623296 doi "https://doi.org/10.1029/2003gl018990" @default.
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