High field strength element/rare earth element fractionation during partial melting in the presence of garnet: Implications for identification of mantle heterogeneities-Reference-Cited by-同舟云学术

High field strength element/rare earth element fractionation during partial melting in the presence of garnet: Implications for identification of mantle heterogeneities

Published:2001-07 Issue:7 Volume:2 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

van Westrenen Wim¹,Blundy Jonathan D.²,Wood Bernard J.²

Affiliation:

1. Geophysical Laboratory; Carnegie Institution of Washington, 5251; Broad Branch Road, Washington, DC 20015 USA

2. Centre for the Experimental and Theoretical Study of the Earth's Interior (CETSEI), Department of Earth Sciences; University of Bristol, Wills Memorial Building; Bristol BS8 1RJ UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference61 articles.

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2. Petrogenesis of Variscan high-temperature group-A eclogites from the Moldanubian zone of the Bohemian Massif, Czechoslovakia;Beard;Contrib. Mineral. Petrol.,1992

3. The distribution of hydroxyl in garnets from the subcontinental mantle of Southern Africa;Bell;Contrib. Mineral. Petrol.,1992

4. Hf isotopic compositions of the Hawaii Scientific Drilling Project core and the source mineralogy of Hawaiian basalts;Blichert-Toft;Geophys. Res. Lett.,1999

5. Prediction of crystal-melt partition coefficients from elastic moduli;Blundy;Nature,1994

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