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Far-field brittle deformation record in the eastern Paris Basin (France)

Published online by Cambridge University Press:  14 October 2022

Thomas Blaise Open the ORCID record for Thomas Blaise [Opens in a new window] ,
Sid Ahmed Ali Khoudja ,
Cédric Carpentier Open the ORCID record for Cédric Carpentier [Opens in a new window] ,
Benjamin Brigaud Open the ORCID record for Benjamin Brigaud [Opens in a new window] ,
Yves Missenard Open the ORCID record for Yves Missenard [Opens in a new window] ,
Xavier Mangenot Open the ORCID record for Xavier Mangenot [Opens in a new window] ,
Philippe Boulvais Open the ORCID record for Philippe Boulvais [Opens in a new window] ,
Philippe Landrein Open the ORCID record for Philippe Landrein [Opens in a new window]  and
Jean Cochard
Thomas Blaise*
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, Orsay 91405, France
Sid Ahmed Ali Khoudja
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, Orsay 91405, France
Cédric Carpentier
Affiliation:
Université de Lorraine, CNRS, GeoRessources, Nancy 54500, France
Benjamin Brigaud
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, Orsay 91405, France
Yves Missenard
Affiliation:
Université Paris-Saclay, CNRS, GEOPS, Orsay 91405, France
Xavier Mangenot
Affiliation:
Caltech, Geological and Planetary Sciences, Pasadena, CA 91106, USA
Philippe Boulvais
Affiliation:
Géosciences Rennes, CNRS, Univ. Rennes, UMR 6118, Rennes F35000, France
Philippe Landrein
Affiliation:
Centre de Meuse/Haute-Marne, Agence Nationale pour La Gestion des Déchets Radioactifs (ANDRA), RD 960, Bure 55290, France
Jean Cochard
Affiliation:
Centre de Meuse/Haute-Marne, Agence Nationale pour La Gestion des Déchets Radioactifs (ANDRA), RD 960, Bure 55290, France
*
Author for correspondence: Thomas Blaise, Email: thomas.blaise@universite-paris-saclay.fr
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Abstract

Jurassic carbonate strata in the eastern Paris Basin exhibit several generations of faults, tension gashes and stylolites. Although their relative chronology can sometimes be determined according to cross-cutting relationships, the duration of major deformation phases and their influence on fluid flow and carbonate cementation are still uncertain. This contribution aims to clarify the timing of brittle deformation and associated calcite cementation. Tension gashes filled by calcite in Jurassic carbonates were sampled in outcrops and boreholes and dated through U–Pb geochronology. Almost all the sampled fractures were cemented during the Cenozoic period. Continuous deformation spread from c. 50 to 30 Ma. Tension gashes oriented N10° to N20° dated at 48–43 Ma show the main Pyrenean contractional stage. A second set of calcites were dated at c. 35–33 Ma and document a Late Eocene – Oligocene extension. A transition from the compressional to the extensional regime is expressed by tension gashes dated between 43 and 35 Ma. Finally, tension gashes oriented N150° to N175°, dated between 32 and 18 Ma, may result from the propagation of the horizontal stress generated by the Alpine orogen or by late Pyrenean deformation. Clumped isotope thermometry on five samples revealed both low crystallization temperatures (from 27 to 53 °C) and the meteoric origin of calcite-precipitating fluids. Our research therefore documents a continuous fracturing from Ypresian to Rupelian times, and less expressed brittle deformation during the Miocene period.

Keywords

calcite U–Pb geochronologyJurassic limestonesParis Basintension gashfar-field deformation
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. 2095 - 2109
Copyright
© The Author(s), 2022. Published by Cambridge University Press

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