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You are here: Home > Library > Diopsidic Cpx produced by assimilation of Fo rich olivine by magmas at Shishaldin Volcano: implications for Alaskan layered complexes

DIOPSIDIC CPX PRODUCED BY ASSIMILATION OF FO RICH OLIVINE BY MAGMAS AT SHISHALDIN VOLCANO: IMPLICATIONS FOR ALASKAN LAYERED COMPLEXES
Fournelle, John, and Marsh, B. D., 1987, Diopsidic Cpx produced by assimilation of Fo rich olivine by magmas at Shishaldin Volcano: implications for Alaskan layered complexes [abs.]: Eos, v. 68, n. 44, p. 1525.
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