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Detailed Reference Information |
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. |
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Keywords
Majorite garnet, Partitioning, Trace elements, Partial melting, Crystal chemistry, Differentiation |
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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. |
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Publisher
Elsevier Science P.O. Box 211 1000 AE Amsterdam The Netherlands (+31) 20 485 3757 (+31) 20 485 3432 nlinfo-f@elsevier.com |
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