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End-Permian mass extinction and palaeoenvironmental changes in Neotethys: Evidence from an oceanic carbonate section in southwestern Tibet
journal contribution
posted on 2010-08-01, 00:00 authored by S Z Shen, C Q Cao, Yichun Zhang, Wenzhong Li, Guang ShiGuang Shi, Y Wang, Y S Wu, K Ueno, C Henderson, X D Wang, H Zhang, X J Wang, J ChenEnd-Permian mass extinction and palaeoenvironmental changes in Neotethys: Evidence from an oceanic carbonate section in southwestern Tibet
History
Journal
Global and planetary changeVolume
73Issue
1-2Pagination
3 - 14Publisher
Elsevier BVLocation
Amsterdam, NetherlandsPublisher DOI
ISSN
0921-8181eISSN
1872-6364Language
engNotes
Available online 14 April 2010Publication classification
C1 Refereed article in a scholarly journalCopyright notice
2010, Elsevier B.V. All rights reserved.Usage metrics
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No categories selectedKeywords
Science & TechnologyPhysical SciencesGeography, PhysicalGeosciences, MultidisciplinaryPhysical GeographyGeologyPermian-Triassicoceanic carbonateNeotethysend-Permian mass extinctionGyanyimaSELONG XISHAN SECTIONTRIASSIC BOUNDARY BEDSSOUTHERN TIBETXIZANG TIBETBRACHIOPOD FAUNACHINAISOTOPESTRATIGRAPHYEVENTRECOVERY
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