Mineralogical changes of the residual solid and trace-element fractionation during partial incongruent melting

Details Mineralogical changes of the residual solid and trace-element fractionation during partial incongruent melting Mineralogical changes of the residual solid and trace-element fractionation during partial incongruent melting

Oct 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992gecoa..56.3705b&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 56, Issue 10, pp.3705-3710

Mathematics

1

Scientific paper

The mathematical expressions presented by and (1976) to treat incongruent melting processes are extended to a more general case where the breakdown of the phases ( ) takes the form 1 + 2 + ... + n = + + + Liq. This modification provides model trace-element fractionation in melts derived from metapelitic rocks, in which muscovite and biotite are always present.

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