Response of a low-subsiding intracratonic basin to long wavelength  deformations: the Palaeocene–early Eocene period in the Paris  Basin

Briais, J.; Guillocheau, F.; Lasseur, E.; Robin, C.; Châteauneuf, J. J.; Serrano, O.

doi:https://doi.org/10.5194/se-7-205-2016

Articles | Volume 7, issue 1

https://doi.org/10.5194/se-7-205-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/se-7-205-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 7, issue 1

Research article

|

08 Feb 2016

Research article |

| 08 Feb 2016

Response of a low-subsiding intracratonic basin to long wavelength deformations: the Palaeocene–early Eocene period in the Paris Basin

J. Briais, F. Guillocheau, E. Lasseur, C. Robin, J. J. Châteauneuf, and O. Serrano

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Final revised paper (published on 08 Feb 2016)
Supplement to the final revised paper
Preprint (discussion started on 07 Dec 2015)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC C1777: 'Revision of the manuscript', Jocelyn BARBARAND, 05 Jan 2016
- AC C1866: 'Reply to Jocelyn Barbarand', Justine Briais, 18 Jan 2016
- AC C1875: 'Reply to Jocelyn Barbarand', Justine Briais, 18 Jan 2016
- AC C1898: 'question for Jocelyn Barbarand', Justine Briais, 20 Jan 2016
RC C1819: 'Review Briais et al.', Anonymous Referee #2, 08 Jan 2016
- AC C1886: 'Reply to anonymous referee', Justine Briais, 18 Jan 2016

Short summary

This paper focuses on the record of lithospheric deformations within an intracratonic basin. This study is based on a detailed analysis of sedimentology and stratigraphy of the Paris Basin (European plate). We identified four intraplate deformations during the Palaeocene-early Eocene period. Age, amplitude, wavelength, and orientation of these deformations are specified and attributed to the geodynamic events. This paper is based on results from J. Briais Phd thesis.