Abstract

Research Article| November 01, 2010 A Permian large igneous province in Tarim and Central Asian orogenic belt, NW China: Results of a ca. 275 Ma mantle plume? Chuan-Lin Zhang; Chuan-Lin Zhang † 1Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China2Nanjing Institute of Geology and Mineral Resources, Nanjing 210016, China †E-mail: zchuanlin@yahoo.com.cn Search for other works by this author on: GSW Google Scholar Zheng-Xiang Li; Zheng-Xiang Li 3Institute for Geoscience Research, Department of Applied Geology, Curtin University of Technology, GPO Box U1987, Perth, WA 6845, Australia Search for other works by this author on: GSW Google Scholar Xian-Hua Li; Xian-Hua Li 4State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China Search for other works by this author on: GSW Google Scholar Yi-Gang Xu; Yi-Gang Xu 1Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China Search for other works by this author on: GSW Google Scholar Gang Zhou; Gang Zhou 5Xinjiang Bureau of Geology and Mineral Resources, Altay 836500, China Search for other works by this author on: GSW Google Scholar Hai-Min Ye Hai-Min Ye 2Nanjing Institute of Geology and Mineral Resources, Nanjing 210016, China4State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China Search for other works by this author on: GSW Google Scholar Author and Article Information Chuan-Lin Zhang † 1Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China2Nanjing Institute of Geology and Mineral Resources, Nanjing 210016, China Zheng-Xiang Li 3Institute for Geoscience Research, Department of Applied Geology, Curtin University of Technology, GPO Box U1987, Perth, WA 6845, Australia Xian-Hua Li 4State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China Yi-Gang Xu 1Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China Gang Zhou 5Xinjiang Bureau of Geology and Mineral Resources, Altay 836500, China Hai-Min Ye 2Nanjing Institute of Geology and Mineral Resources, Nanjing 210016, China4State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China †E-mail: zchuanlin@yahoo.com.cn Publisher: Geological Society of America Received: 09 Jan 2009 Revision Received: 17 Oct 2009 Accepted: 20 Oct 2009 First Online: 08 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 © 2010 Geological Society of America GSA Bulletin (2010) 122 (11-12): 2020–2040. https://doi.org/10.1130/B30007.1 Article history Received: 09 Jan 2009 Revision Received: 17 Oct 2009 Accepted: 20 Oct 2009 First Online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Chuan-Lin Zhang, Zheng-Xiang Li, Xian-Hua Li, Yi-Gang Xu, Gang Zhou, Hai-Min Ye; A Permian large igneous province in Tarim and Central Asian orogenic belt, NW China: Results of a ca. 275 Ma mantle plume?. GSA Bulletin 2010;; 122 (11-12): 2020–2040. doi: https://doi.org/10.1130/B30007.1 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 SocietyGSA Bulletin Search Advanced Search Abstract New sensitive high-resolution ion microprobe (SHRIMP) U-Pb zircon ages, geochemical data, and a synthesis of existing stratigraphic, geochronologic, and geochemical results from the Tarim block and the Central Asian orogenic belt in northwestern China suggest the presence of a Permian (ca. 275 Ma) large igneous province (the Bachu large igneous province). The large igneous province consists predominantly of coeval mafic rocks (basalts and mafic-ultramafic intrusions) having an aerial coverage of more than 600,000 km2, and its formation was accompanied by voluminous emplacement of A-type granites. This large igneous province, interpreted to be of mantle plume origin, is ∼15 m.y. older than the ca. 260 Ma Emeishan large igneous province in southwestern China and ∼25 m.y. older than the 251 Ma Siberian Trap in Russia. Such a sudden flair up of plume activity in the Permian may represent the early stage of the Pangean superplume event. The Permian plumes likely played a role in late Paleozoic rapid continental crustal growth in the Central Asian orogenic belt. In addition, there appear to be two types of mantle geochemical provinces (domains) in the region, a long-term enriched Tarim province and a subduction-metasomatized and depleted Central Asian orogenic belt province. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call