Evidence from high-Ni olivines for a hybridized peridotite/pyroxenite source for orogenic andesites from the central Mexican Volcanic Belt

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Straub SM, A.B. LG, A.L. M-DP, Langmuir CH. Evidence from high-Ni olivines for a hybridized peridotite/pyroxenite source for orogenic andesites from the central Mexican Volcanic Belt. Geochem. Geophys. Geosyst. 2008;9 (3).

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Last updated on 12/14/2018

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