Influence of subsolidus processes on the chromium number in spinel in ultramafic rocks

Author:

Voigt Martin,von der Handt Anette

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference68 articles.

1. Allan JF, Sack RO, Batiza R (1988) Cr-rich spinels as petrogenetic indicators; MORB-type lavas from the Lamont seamount chain, eastern Pacific. Am Mineral 73(7-8):741–753

2. Asimow PD, Ghiorso MS (1998) Algorithmic modifications extending MELTS to calculate subsolidus phase relations. Am Mineral 83:1127–1132

3. Baker MB, Stolper EM (1994) Determining the composition of high-pressure mantle melts using diamond aggregates. Geochim Cosmochim Acta 58(13):2811–2827

4. Barnes SJ, Roeder PL (2001) The range of spinel compositions in terrestrial mafic and ultramafic rocks. J Petrol 42(12):2279–2302

5. Bodinier JL, Dupuy C, Dostal J, Merlet C (1987) Distribution of trace transition elements in olivine and pyroxenes from ultramafic xenoliths; application of microprobe analysis. Am Mineral 72(9–10):902–913

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