(Q57857333)

English

Experimental determination of trace element partitioning between garnet and silica-rich liquid during anhydrous partial melting of MORB-like eclogite

article by M. Pertermann et al published May 2004 in G3: Geochemistry, Geophysics, Geosystems

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scholarly article

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Experimental determination of trace element partitioning between garnet and silica-rich liquid during anhydrous partial melting of MORB-like eclogite (English)

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mid-ocean ridge basalt

object named as

MORB

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based on heuristic

inferred from title

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based on heuristic

inferred from title

Marc M. Hirschmann

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object named as

M. M. Hirschmann

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author name string

M. Pertermann

1

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K. Hametner

3

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D. Günther

4

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M. W. Schmidt

5

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publication date

May 2004

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G3: Geochemistry, Geophysics, Geosystems

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5

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5

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1 reference

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1 reference

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The composition of the Earth

1 reference

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1 reference

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Anhydrous Partial Melting Experiments on MORB-like Eclogite: Phase Relations, Phase Compositions and Mineral-Melt Partitioning of Major Elements at 2-3 GPa

1 reference

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1 reference

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1 reference

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Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions

1 reference

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7 January 2021

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1 reference

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based on heuristic

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Melting experiments on anhydrous peridotite KLB-1: Compositions of magmas in the upper mantle and transition zone

1 reference

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based on heuristic

inferred from DOI database lookup

Identifiers

10.1029/2003GC000638

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2004GGG.....5.5A01P

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