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• W2029403887 abstract "Research Article| May 01, 1995 Permian-Carboniferous and Permian-Triassic magmatism in the rift zone bordering the Tethyan margin of southern Pangea J. J. Veevers; J. J. Veevers 1Australian Plate Research Group, School of Earth Sciences, Macquarie University, North Ryde, New South Wales 2109, Australia Search for other works by this author on: GSW Google Scholar R. C. Tewari R. C. Tewari 2Dharma Samaj College, Aligarh, Uttar Pradesh, 200201, India Search for other works by this author on: GSW Google Scholar Author and Article Information J. J. Veevers 1Australian Plate Research Group, School of Earth Sciences, Macquarie University, North Ryde, New South Wales 2109, Australia R. C. Tewari 2Dharma Samaj College, Aligarh, Uttar Pradesh, 200201, India 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 (5): 467–470. https://doi.org/10.1130/0091-7613(1995)023<0467:PCAPTM>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 MailTo Tools Icon Tools Get Permissions Search Site Citation J. J. Veevers, R. C. Tewari; Permian-Carboniferous and Permian-Triassic magmatism in the rift zone bordering the Tethyan margin of southern Pangea. Geology 1995;; 23 (5): 467–470. doi: https://doi.org/10.1130/0091-7613(1995)023<0467:PCAPTM>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 Magma was emplaced in the India-Australia rift zone along the Tethyan margin during Permian-Carboniferous and Permian-Triassic time. Permian-Carboniferous alkalic granite and basaltic and rhyolitic lava flows and tuffs formed at the same time as right-lateral transtension of Pangea, as recorded by the magmatic rocks of neocratonic post-Variscan Europe and post-Kanimblan eastern Australia. Permian-Triassic tholeiitic basalt in India, alkalic magmatic rocks in Oman, and rhyolite, dolerite, and undersaturated alkalic volcanic rocks in Western Australia preceded and accompanied the early opening of the Neo-Tethys ocean. Coeval magmatism included the voluminous mid-plate Siberian Traps, the Emeishan Basalt of south China, and the peak activity of the magmatic arc along the convergent Panthalassan margin. The background magmatism probably permitted the Siberian Traps to trigger the environmental catastrophe at the Permian-Triassic boundary. 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." @default.
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• W2029403887 title "Permian-Carboniferous and Permian-Triassic magmatism in the rift zone bordering the Tethyan margin of southern Pangea" @default.
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