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How sensitive are intraplate inherited structures? Insight from the Cévennes Fault System (Languedoc, SE France)

Published online by Cambridge University Press:  11 April 2022

Oriane Parizot Open the ORCID record for Oriane Parizot [Opens in a new window] ,
Yves Missenard Open the ORCID record for Yves Missenard [Opens in a new window] ,
Jocelyn Barbarand Open the ORCID record for Jocelyn Barbarand [Opens in a new window] ,
Thomas Blaise Open the ORCID record for Thomas Blaise [Opens in a new window] ,
Antonio Benedicto Open the ORCID record for Antonio Benedicto [Opens in a new window] ,
Frederic Haurine Open the ORCID record for Frederic Haurine [Opens in a new window]  and
Philippe Sarda Open the ORCID record for Philippe Sarda [Opens in a new window]
Oriane Parizot
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, 91405, Orsay, France
Yves Missenard*
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, 91405, Orsay, France
Jocelyn Barbarand
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, 91405, Orsay, France
Thomas Blaise
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, 91405, Orsay, France
Antonio Benedicto
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, 91405, Orsay, France
Frederic Haurine
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, 91405, Orsay, France
Philippe Sarda
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, 91405, Orsay, France
*
Author for correspondence: Yves Missenard, Email: yves.missenard@universite-paris-saclay.fr
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Abstract

Deformation in intraplate domains is usually considered as a consequence of tectonic events at plate boundaries. Nevertheless, the occurrence of intraplate earthquakes such as the recent Le Teil event in the south of France along the Cévennes Fault System (CFS), on 11 November 2019, Mw = 4.9, questions whether this far-field deformation only occurs during tectonic pulses at plate boundaries, or if it corresponds to low-intensity but regional continuous deformation through time. To address this question, we have coupled U–Pb geochronology of fault-related calcites with structural analysis along a major fault system (the CFS) in the South-East Basin, France. We evidence (1) an Albian activity of the CFS and (2) a continuous compressional activity of the CFS and satellite structures during the whole Eocene and probably during the Late Cretaceous – Palaeocene, including periods (e.g. Lutetian) usually considered as phases of tectonic quiescence. We thus demonstrate that the tectonic reactivation of this intraplate fault system is not restricted to periods of high rates of deformation at plate boundaries.

Keywords

intraplate deformationPyreneesCévennes Fault SystemU–Pb geochronologyfault-related calciteLA-ICP-MS
Type
ABSOLUTE DATING OF FAULTS AND FRACTURES
Information
Geological Magazine , Volume 159 , Issue 11-12: THEMATIC ISSUE: Faults and fractures in rocks: mechanics, occurrence, dating, stress history and fluid flow , November 2022 , pp. 2082 - 2094
Copyright
© The Author(s), 2022. Published by Cambridge University Press

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