U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin
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. Constraining the timing of brittle faulting is critical in understanding crustal...
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Format: | Article in Journal/Newspaper |
Language: | English |
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Geological Society of America
2016
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Online Access: | http://geology.gsapubs.org/content/44/7/531 http://hdl.handle.net/2381/37752 https://doi.org/10.1130/G37868.1 |
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ftleicester:oai:lra.le.ac.uk:2381/37752 2023-05-15T16:10:55+02:00 U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin Roberts, Nick M. W. Walker, Richard J. 2016-06-14T12:32:28Z http://geology.gsapubs.org/content/44/7/531 http://hdl.handle.net/2381/37752 https://doi.org/10.1130/G37868.1 en eng Geological Society of America Geology (Boulder), 2016, 44 (7), pp. 531-534 0091-7613 http://geology.gsapubs.org/content/44/7/531 http://hdl.handle.net/2381/37752 doi:10.1130/G37868.1 1943-2682 Copyright © 2016 Geological Society of America. Deposited with reference to the publisher’s archiving policy available on the SHERPA/RoMEO website. Journal Article Article 2016 ftleicester https://doi.org/10.1130/G37868.1 2019-03-22T20:21:45Z 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. 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. Peer-reviewed Post-print Article in Journal/Newspaper Faroe Islands Northeast Atlantic University of Leicester: Leicester Research Archive (LRA) Faroe Islands Geology 44 7 531 534 |
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Open Polar |
collection |
University of Leicester: Leicester Research Archive (LRA) |
op_collection_id |
ftleicester |
language |
English |
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. 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. Peer-reviewed Post-print |
format |
Article in Journal/Newspaper |
author |
Roberts, Nick M. W. Walker, Richard J. |
spellingShingle |
Roberts, Nick M. W. Walker, Richard J. U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin |
author_facet |
Roberts, Nick M. W. Walker, Richard J. |
author_sort |
Roberts, Nick M. W. |
title |
U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin |
title_short |
U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin |
title_full |
U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin |
title_fullStr |
U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin |
title_full_unstemmed |
U-Pb geochronology of calcite-mineralized faults: Absolute timing of rift-related fault events on the northeast Atlantic margin |
title_sort |
u-pb geochronology of calcite-mineralized faults: absolute timing of rift-related fault events on the northeast atlantic margin |
publisher |
Geological Society of America |
publishDate |
2016 |
url |
http://geology.gsapubs.org/content/44/7/531 http://hdl.handle.net/2381/37752 https://doi.org/10.1130/G37868.1 |
geographic |
Faroe Islands |
geographic_facet |
Faroe Islands |
genre |
Faroe Islands Northeast Atlantic |
genre_facet |
Faroe Islands Northeast Atlantic |
op_relation |
Geology (Boulder), 2016, 44 (7), pp. 531-534 0091-7613 http://geology.gsapubs.org/content/44/7/531 http://hdl.handle.net/2381/37752 doi:10.1130/G37868.1 1943-2682 |
op_rights |
Copyright © 2016 Geological Society of America. Deposited with reference to the publisher’s archiving policy available on the SHERPA/RoMEO website. |
op_doi |
https://doi.org/10.1130/G37868.1 |
container_title |
Geology |
container_volume |
44 |
container_issue |
7 |
container_start_page |
531 |
op_container_end_page |
534 |
_version_ |
1765996053749825536 |