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Detailed Reference Information
Corgne & Wood 2004
Corgne, A. and Wood, B.J. (2004). Trace element partitioning between majoritic garnet and silicate melt at 25 GPa. Physics of the Earth and Planetary Interiors 143-144: 407-419. doi: 10.1016/j.pepi.2003.08.012.
Keywords
Majorite garnet, Partitioning, Trace elements, Partial melting, Crystal chemistry, Differentiation
Project -- G-cubed.org Themes -- Phase Relations and Trace Element Partitioning on the Mantle Solidus
This theme, which grew out of a 1999 Fall AGU special session, brings together papers by experimentalists and geochemists concerned with the conditions under which melting occurs in the Earth's mantle and the mineral-melt partitioning of trace elements under those condition.
Journal
Physics of the Earth and Planetary Interiors
http://www.elsevier.com/locate/pepi
Publisher
Elsevier Science
P.O. Box 211
1000 AE Amsterdam
The Netherlands
(+31) 20 485 3757
(+31) 20 485 3432
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