Heat flow study of the Emeishan large igneous province region: Implications for the geodynamics of the Emeishan mantle plume
Abstract
The Emeishan large igneous province (ELIP) is widely considered to be a consequence of a mantle plume. The supporting evidence includes rapid emplacement, voluminous flood basalt eruptions, and high mantle potential temperature estimates. Several studies have suggested that there was surface uplift prior to the eruption of the Emeishan flood basalts. Additionally, the plume's lateral extent is hard to constrain and has been variously estimated...
Paper Details
Title
Heat flow study of the Emeishan large igneous province region: Implications for the geodynamics of the Emeishan mantle plume
Published Date
Jan 1, 2018
Journal
Volume
724-725
Pages
11 - 27
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