(Q57857355)

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High-pressure partial melting of garnet pyroxenite: possible mafic lithologies in the source of ocean island basalts

article by Tetsu Kogiso et al published December 2003 in Earth and Planetary Science Letters

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High-pressure partial melting of garnet pyroxenite: possible mafic lithologies in the source of ocean island basalts (English)

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Tetsu Kogiso

1

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Marc M. Hirschmann

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Marc M Hirschmann

series ordinal

2

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Daniel J. Frost

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Daniel J Frost

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3

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language of work or name

English

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publication date

December 2003

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published in

Earth and Planetary Science Letters

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volume

216

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issue

4

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page(s)

603-617

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cites work

Partial melting experiments on a MORB-like pyroxenite between 2 and 3 GPa: Constraints on the presence of pyroxenite in basalt source regions from solidus location and melting rate

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7 January 2021

Experimental melting studies on a model upper mantle composition at high pressure under water-saturated and water-undersaturated conditions

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7 January 2021

The role of CO2 in the genesis of olivine melilitite

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7 January 2021

Systematic study of liquidas phase relations in olivine melilitite +H2O +CO2 at high pressures and petrogenesis of an olivine melilitite magma

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7 January 2021

Major-element variability in the Hawaiian mantle plume

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7 January 2021

Osmium isotopes and mantle convection

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7 January 2021

Length scales of mantle heterogeneities and their relationship to ocean island basalt geochemistry

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reference URL

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retrieved

7 January 2021

A possible role for garnet pyroxenite in the origin of the "garnet signature" in MORB

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7 January 2021

Dehydration Melting of Metabasalt at 8-32 kbar: Implications for Continental Growth and Crust-Mantle Recycling

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7 January 2021

Implications of a two-component marble-cake mantle

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7 January 2021

Mixing and the distribution of heterogeneities in a chaotically convecting mantle

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7 January 2021

Diffusion in Mg2SiO4 polymorphs and chemical heterogeneity in the mantle transition zone

1 reference

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7 January 2021

On the conditions for lower crustal convective instability

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7 January 2021

Incompatible trace elements in OIB and MORB and source enrichment in the sub-oceanic mantle

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7 January 2021

Majorite fractionation recorded in the geochemistry of peridotites from South Africa

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7 January 2021

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

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retrieved

7 January 2021

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inferred from DOI database lookup

The solubility of quartz in H2O in the lower crust and upper mantle

1 reference

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reference URL

https://ui.adsabs.harvard.edu/abs/1994GeCoA..58.4831M/citations

retrieved

21 January 2023

Identifiers

DOI

10.1016/S0012-821X(03)00538-7

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ADS bibcode

2003E&PSL.216..603K

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(Q57857355)

High-pressure partial melting of garnet pyroxenite: possible mafic lithologies in the source of ocean island basalts

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