Partitioning of elements between silicate melt and H2ONaCl fluids at 1.5 and 2.0 GPa pressure: Implications for mantle metasomatism-Reference-Cited by-同舟云学术

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Partitioning of elements between silicate melt and H2ONaCl fluids at 1.5 and 2.0 GPa pressure: Implications for mantle metasomatism

Published:1995-10 Issue:20 Volume:59 Page:4237-4246
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Ayers John C.,Eggler David H.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference46 articles.

1. The solubility of quartz in supercritical water;Anderson;Amer. J. Sci.,1965

2. The trapped fluid phase in upper mantle xenoliths from Victoria, Australia: Implications for mantle metasomatism;Anderson;Contrib. Mineral. Petrol.,1984

3. Partitioning of elements between silicate melts and salt water at mantle conditions;Ayers,1988

4. Partitioning of trace elements between silicate melts and H2ONaCl fluids at upper mantle pressures and temperatures;Ayers,1988

5. A new capsule technique for hydrothermal experiments using the piston-cylinder apparatus;Ayers;Amer. Mineral.,1992

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