Oxidation zonation within the Emeishan large igneous province: Evidence from mantle-derived syenitic plutons
Abstract
The mantle-derived felsic plutonic rocks of the Emeishan large igneous province consist of peralkaline and metaluminous varieties. The peralkaline rocks appear to be formed by fractional crystallization of mafic magmas whereas the metaluminous plutonic rocks appear to be derived by partial melting of underplated mafic rocks. The metaluminous Woshui pluton is 259.6 ± 0.5 Ma and contains alkali feldspar, clinopyroxene, magnesiohornblende,...
Paper Details
Title
Oxidation zonation within the Emeishan large igneous province: Evidence from mantle-derived syenitic plutons
Published Date
Aug 1, 2012
Volume
54-55
Pages
31 - 40
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