Chromian spinel–olivine phase chemistry and the origin of primitive basalts of the southern Washington Cascades

Author:

Smith D.R.,Leeman W.P.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference71 articles.

1. How deep do common basaltic magmas form and differentiate?;Albarède;Journal of Geophysical Research,1992

2. Cr-rich spinels as petrogenetic indicators; MORB-type lavas from the Lamont seamount chain, eastern Pacific;Allan;American Mineralogist,1988

3. Compositional variation of olivine–chromian spinel in Mg-rich magmas as a guide to their residual spinel peridotites;Arai;Journal of Volcanology and Geothermal Research,1994

4. Primitive magmas at five Cascade volcanic fields; melts from hot, heterogeneous sub-arc mantle;Bacon;Canadian Mineralogist,1997

5. Determining the composition of high-pressure mantle melts using diamond aggregates;Baker;Geochimica et Cosmochimica Acta,1994

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