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• W2415501186 abstract "Research Article| July 01, 2016 U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin Nick M.W. Roberts; Nick M.W. Roberts 1NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth NG12 5GG, UK Search for other works by this author on: GSW Google Scholar Richard J. Walker Richard J. Walker 2Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK Search for other works by this author on: GSW Google Scholar Author and Article Information Nick M.W. Roberts 1NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth NG12 5GG, UK Richard J. Walker 2Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK Publisher: Geological Society of America Received: 07 Mar 2016 Revision Received: 16 May 2016 Accepted: 19 May 2016 First Online: 02 Jun 2017 Online Issn: 1943-2682 Print Issn: 0091-7613 © 2016 Geological Society of America Geology (2016) 44 (7): 531–534. https://doi.org/10.1130/G37868.1 Article history Received: 07 Mar 2016 Revision Received: 16 May 2016 Accepted: 19 May 2016 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 Nick M.W. Roberts, Richard J. Walker; U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin. Geology 2016;; 44 (7): 531–534. doi: https://doi.org/10.1130/G37868.1 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 Constraining the timing of brittle faulting is critical in understanding crustal deformation and fluid flow, but many regional-scale fault systems lack readily available techniques to provide absolute chronological information. Calcite mineralization occurs in crustal faults in many geological settings and can be suitable for U-Pb geochronology. This application has remained underutilized because traditional bulk dissolution techniques require uncommonly high U concentration. Because U and Pb are distributed heterogeneously throughout calcite crystals, high-spatial-resolution sampling techniques can target domains with high U and variable U/Pb ratios. Here we present a novel application of in-situ laser ablation–inductively coupled plasma–mass spectrometry (LA-ICP-MS) to basaltic fault rock geochronology in the Faroe Islands, northeast Atlantic margin. Faults that are kinematically linked to deformation associated with continental break-up were targeted. Acquired ages for fault events range from mid-Eocene to mid-Miocene and are therefore consistently younger than the regional early Eocene onset of ocean spreading, highlighting protracted brittle deformation within the newly developed continental margin. Calcite geochronology from LA-ICP-MS U-Pb analysis represents an important and novel method to constrain the absolute timing of fault and fluid-flow events. 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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• W2415501186 title "U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin" @default.
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