The Emeishan Flood Basalt in SW China: a mantle plume initiation model and its connection with continental breakup and mass extinction at the Permian-Triassic boundary. In M. Flower et al. (eds.) Mantle Dynamics and Plate Interactions in

Chung, S.L.S.L.ChungJahn, B.M.B.M.JahnWu, G.Y.G.Y.WuLo, C.H.C.H.LoCong, B.L.B.L.Cong2010-09-282018-06-282010-09-282018-06-281998-11http://ntur.lib.ntu.edu.tw//handle/246246/206699en-USThe Emeishan Flood Basalt in SW China: a mantle plume initiation model and its connection with continental breakup and mass extinction at the Permian-Triassic boundary. In M. Flower et al. (eds.) Mantle Dynamics and Plate Interactions injournal article