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Vein calcite dating reveals Pyrenean orogen as cause of Paleogene deformation in southern England

View ORCID ProfileRandall R. Parrish, Claire M. Parrish and Stephanie Lasalle
Journal of the Geological Society, 175, 425-442, 8 February 2018, https://doi.org/10.1144/jgs2017-107
Randall R. Parrish
1School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, UK
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Claire M. Parrish
264 Buckingham Road, Brighton BN1 3RQ, UK
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Stephanie Lasalle
1School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, UK
3Research & Innovation Services, University of Portsmouth, 28 Guildhall Walk, Portsmouth PO1 2DD, UK
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Abstract

An improved method of U–Pb dating of vein calcite formed during deformation is used to determine the age and cause of folding along the south coast of England. Fractures arising from folding of Late Cretaceous Chalk of southern England occurred 34.7 ± 1.7 myr ago. Underlying Jurassic strata have veins within fractures with ages of 55, 48–42, 39–37, 34–31 and 25 Ma, with 34–31 Ma being the tectonic culmination. Folding was slightly younger than the age of the youngest strata in the overlying Solent Group, suggesting that folding terminated basin sedimentation. This age of north–south shortening is inconsistent with attribution to intraplate forces from the mainly younger Alps, but is plausibly a result of the Pyrenean Orogen, which evolved from 50 to 28 myr ago with a late Eocene culmination. A modified method for carbonate laser ablation inductively coupled plasma mass spectrometry U–Pb dating is presented that uses measured 232Th and 208Pb as a better monitor of common Pb, and it has distinct advantages over existing methods. Initial common lead determined on samples conforms closely to model compositions calculated by earlier workers, with free regressions giving the most robust dates. The modified method is applicable to structural geology, carbonate diagenesis and to dating of carbonate relevant to palaeo-environmental and archaeological studies.

Supplementary material: Details of sample locations and characteristics, photographs of sample localities, microscopic images of veins, details of the experimental procedure and U–Pb data for all samples and reference materials are available at https://doi.org/10.6084/m9.figshare.c.3997086

  • © 2018 The Author(s)
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Journal of the Geological Society: 175 (3)
Journal of the Geological Society
Volume 175, Issue 3
May 2018
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Vein calcite dating reveals Pyrenean orogen as cause of Paleogene deformation in southern England

Randall R. Parrish, Claire M. Parrish and Stephanie Lasalle
Journal of the Geological Society, 175, 425-442, 8 February 2018, https://doi.org/10.1144/jgs2017-107
Randall R. Parrish
1School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, UK
  • Find this author on Google Scholar
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  • Search for this author on this site
  • ORCID record for Randall R. Parrish
  • For correspondence: randall.parrish@port.ac.uk
Claire M. Parrish
264 Buckingham Road, Brighton BN1 3RQ, UK
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
Stephanie Lasalle
1School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, UK
3Research & Innovation Services, University of Portsmouth, 28 Guildhall Walk, Portsmouth PO1 2DD, UK
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Vein calcite dating reveals Pyrenean orogen as cause of Paleogene deformation in southern England

Randall R. Parrish, Claire M. Parrish and Stephanie Lasalle
Journal of the Geological Society, 175, 425-442, 8 February 2018, https://doi.org/10.1144/jgs2017-107
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  • Article
    • Abstract
    • Strata, structural geology and vein descriptions
    • U–Pb dating strategy, method and derivation of common lead corrected ages
    • Results
    • Discussion
    • The cause of Eocene and Oligocene deformation
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