Please use this identifier to cite or link to this item: http://hdl.handle.net/2381/37752
Title: U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin
Authors: Roberts, Nick M. W.
Walker, Richard J.
First Published: 1-Jun-2016
Publisher: Geological Society of America
Citation: Geology (Boulder), 2016, 44 (7), pp. 531-534
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.
DOI Link: 10.1130/G37868.1
ISSN: 0091-7613
eISSN: 1943-2682
Links: http://geology.gsapubs.org/content/44/7/531
http://hdl.handle.net/2381/37752
Embargo on file until: 1-Jun-2017
Version: Post-print
Status: Peer-reviewed
Type: Journal Article
Rights: Copyright © 2016 Geological Society of America. Deposited with reference to the publisher’s archiving policy available on the SHERPA/RoMEO website.
Description: The file associated with this record is under a 12-month embargo from publication in accordance with the publisher's self-archiving policy. The full text may be available through the publisher links provided above.
Appears in Collections:Published Articles, Dept. of Geology

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