(Q107275421)

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Melting experiments on anhydrous peridotite KLB-1 from 5.0 to 22.5 GPa

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Melting experiments on anhydrous peridotite KLB-1 from 5.0 to 22.5 GPa (English)

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author name string

Jianzhong Zhang

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1

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Claude Herzberg

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2

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publication date

10 September 1994

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published in

Journal of Geophysical Research

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volume

99

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issue

B9

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page(s)

17729-17742

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cites work

Crystal chemistry of phase B and an anhydrous analogue: implications for water storage in the upper mantle

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Melting of Ferromagnesian Silicates Under the Lower Mantle Conditions

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Melting of peridotite at uppermost lower-mantle conditions

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Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications

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Experimental determination of element partitioning between silicate perovskites, garnets and liquids: constraints on early differentiation of the mantle

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The system Mg2SiO4-Fe2SiO4at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel

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Are Ocean Floor Basalts Primary Magma?

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Melting of peridotite to 14 GPa and the genesis of komatiite

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Partitioning “equilibrium”, temperature gradients, and constraints on Earth differentiation

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Melting of (Mg, Fe)SiO3-Perovskite to 625 Kilobars: Indication of a High Melting Temperature in the Lower Mantle

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(Q107275421)

Melting experiments on anhydrous peridotite KLB-1 from 5.0 to 22.5 GPa

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