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Picritic lava flows near Lijiang in the late Permian Emeishan flood basalt province are associated with augite-phyric basalt, aphyric basalt, and basaltic pyroclastic units. The dominant phenocryst in the picritic flows is Mg-rich olivine (up to 91·6% forsterite component) with high CaO contents (to 0·42 wt %) and glass inclusions, indicating that the olivine crystallized from a melt. Associated c...

Geochemistry of Picritic and Associated Basalt Flows of the Western Emeishan Flood Basalt Province, China