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• W2330645900 abstract "Research Article| December 01, 2012 U-Pb zircon crystallization age of the Muslim Bagh ophiolite: Enigmatic remains of an extensive pre-Himalayan arc M. Ishaq Kakar; M. Ishaq Kakar 1Centre of Excellence in Mineralogy, University of Balochistan, Quetta, Pakistan Search for other works by this author on: GSW Google Scholar Alan S. Collins; Alan S. Collins * 2Tectonics, Resources and Exploration (TRaX), School of Earth and Environmental Sciences, University of Adelaide, SA 5005, Australia *E-mail: alan.collins@adelaide.edu.au. Search for other works by this author on: GSW Google Scholar Khalid Mahmood; Khalid Mahmood 1Centre of Excellence in Mineralogy, University of Balochistan, Quetta, Pakistan Search for other works by this author on: GSW Google Scholar John D. Foden; John D. Foden 2Tectonics, Resources and Exploration (TRaX), School of Earth and Environmental Sciences, University of Adelaide, SA 5005, Australia Search for other works by this author on: GSW Google Scholar Mehrab Khan Mehrab Khan 3Department of Geology, University of Balochistan, Quetta, Pakistan Search for other works by this author on: GSW Google Scholar Author and Article Information M. Ishaq Kakar 1Centre of Excellence in Mineralogy, University of Balochistan, Quetta, Pakistan Alan S. Collins * 2Tectonics, Resources and Exploration (TRaX), School of Earth and Environmental Sciences, University of Adelaide, SA 5005, Australia Khalid Mahmood 1Centre of Excellence in Mineralogy, University of Balochistan, Quetta, Pakistan John D. Foden 2Tectonics, Resources and Exploration (TRaX), School of Earth and Environmental Sciences, University of Adelaide, SA 5005, Australia Mehrab Khan 3Department of Geology, University of Balochistan, Quetta, Pakistan *E-mail: alan.collins@adelaide.edu.au. Publisher: Geological Society of America Received: 03 Feb 2012 Revision Received: 14 May 2012 Accepted: 27 May 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2012 Geological Society of America Geology (2012) 40 (12): 1099–1102. https://doi.org/10.1130/G33270.1 Article history Received: 03 Feb 2012 Revision Received: 14 May 2012 Accepted: 27 May 2012 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation M. Ishaq Kakar, Alan S. Collins, Khalid Mahmood, John D. Foden, Mehrab Khan; U-Pb zircon crystallization age of the Muslim Bagh ophiolite: Enigmatic remains of an extensive pre-Himalayan arc. Geology 2012;; 40 (12): 1099–1102. doi: https://doi.org/10.1130/G33270.1 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 SocietyGeology Search Advanced Search Abstract The pre-Himalayan evolution of Tethys is fundamental in interpreting the significance of India’s Paleogene deceleration and the timing of the India-Eurasia collision—the archetype continental collision that governs our understanding of collisional processes. Here we date zircons from plagiogranite sheeted dikes in the Muslim Bagh ophiolite that yield a U-Pb age of 80.2 ± 1.5 Ma. This age is interpreted as dating the crystallization of plagiogranites that occur at the top of gabbro plutons as well as within sheeted dikes. These represent highly fractionated magma chamber differentiates. The plagiogranite’s trace element abundances are typical of subduction petrogenesis and can be explained by the addition of slab-derived components to a depleted mantle wedge. Muslim Bagh ophiolite formation was coeval with the Spongtang Arc in a similar tectonic environment. We interpret the chain of ophiolites within western Pakistan as corollaries of the Spongtang Arc that formed ∼15 Ma before they were obducted on the Indian passive margin. These form an extensive arc system that developed as oceanic crust in Tethys foundered during India’s migration north. Latest Maastrichtian ophiolite-sole formation and subsequent Paleocene obduction of the arc onto India was the first arc-India collision—a herald of the collisions to come later. 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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• W2330645900 title "U-Pb zircon crystallization age of the Muslim Bagh ophiolite: Enigmatic remains of an extensive pre-Himalayan arc" @default.
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