Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary

Research Article| October 01, 1995 Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary Sun-Lin Chung; Sun-Lin Chung 1Department of Geology, National Taiwan University, Taipei, Taiwan, Republic of China Search for other works by this author on: GSW Google Scholar Bor-ming Jahn Bor-ming Jahn 2Géosciences Rennes, Université de Rennes 1, F-35042 Rennes Cedex, France Search for other works by this author on: GSW Google Scholar Author and Article Information Sun-Lin Chung 1Department of Geology, National Taiwan University, Taipei, Taiwan, Republic of China Bor-ming Jahn 2Géosciences Rennes, Université de Rennes 1, F-35042 Rennes Cedex, France Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1995) 23 (10): 889–892. https://doi.org/10.1130/0091-7613(1995)023<0889:PLIIGO>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Sun-Lin Chung, Bor-ming Jahn; Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary. Geology 1995;; 23 (10): 889–892. doi: https://doi.org/10.1130/0091-7613(1995)023<0889:PLIIGO>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The Emeishan flood volcanism that erupted at Permian-Triassic boundary time produced a large igneous province of at least 2.5 X 105 km2 in the western margin of the Yangtze craton, southwestern China. The volcanic successions, suggested to have resulted from a starting mantle plume, comprise thick piles of basaltic flows and subordinate picrites and pyroclastics. The picrites, which have high magnesian contents (MgO ≊ 20–16 wt%), variable degrees of light rare earth element enrichment [(Ce/Yb)N ≊ 4–25] and heterogeneous isotope ratios [ϵNd ≊ (T) +4 to −4], are proposed to have been generated by mixing between the dominant plume-derived magmas and small amounts of lamproitic liquids from the continental lithospheric mantle. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.