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• W2078902477 abstract "Research Article| August 01, 2008 Initiation of Franciscan subduction along a large-offset fracture zone: Evidence from mantle peridotites, Stonyford, California Sung Hi Choi; Sung Hi Choi 1Korea Polar Research Institute, Songdo Techno Park 7-50, Incheon 406-840, South Korea Search for other works by this author on: GSW Google Scholar Samuel B. Mukasa; Samuel B. Mukasa * 2Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1005, USA *E-mail: mukasa@umich.edu. Search for other works by this author on: GSW Google Scholar John W. Shervais John W. Shervais 3Department of Geology, Utah State University, Logan, Utah 84322-4505, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Sung Hi Choi 1Korea Polar Research Institute, Songdo Techno Park 7-50, Incheon 406-840, South Korea Samuel B. Mukasa * 2Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1005, USA John W. Shervais 3Department of Geology, Utah State University, Logan, Utah 84322-4505, USA *E-mail: mukasa@umich.edu. Publisher: Geological Society of America Received: 08 Nov 2007 Revision Received: 26 Mar 2008 Accepted: 30 Mar 2008 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2008 Geological Society of America Geology (2008) 36 (8): 595–598. https://doi.org/10.1130/G24993A.1 Article history Received: 08 Nov 2007 Revision Received: 26 Mar 2008 Accepted: 30 Mar 2008 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Sung Hi Choi, Samuel B. Mukasa, John W. Shervais; Initiation of Franciscan subduction along a large-offset fracture zone: Evidence from mantle peridotites, Stonyford, California. Geology 2008;; 36 (8): 595–598. doi: https://doi.org/10.1130/G24993A.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 We report here on the radiogenic isotope characteristics of peridotites from one ophiolite locale, Stonyford, in the Coast Range ophiolite (CRO) of California, spanning the entire observed range of upper mantle peridotites from both abyssal and subduction-zone settings. Based on the Sr-Nd-Pb-Hf isotopic compositions and estimated equilibration temperatures, we suggest that the abyssal peridotite block represents a remnant of large-offset transform oceanic lithosphere at >172 Ma. East-dipping, proto-Franciscan subduction is likely to have been initiated along this fault zone during a plate reorganization event, which produced the supra-subduction zone (SSZ) peridotites in the CRO. We propose that the remnant abyssal peridotites represent a snapshot of the mantle wedge composition prior to overprinting of large sectors by hydrous melting during the subsequent subduction-controlled SSZ processes. 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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• W2078902477 title "Initiation of Franciscan subduction along a large-offset fracture zone: Evidence from mantle peridotites, Stonyford, California" @default.
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