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Une méthode de quantification de la dégradation d'un escarpement de faille au cours des cycles climatiques du Quaternaire : la faille de Jobourg (Nord Cotentin, France).

Abstract : The degradation of the Jobourg fault-scarp occurred by cryoclastic processes in a periglacial environment during a part of Quaternary time. An attempt of quantification indicates a bulk scarp erosion of about 39 m3 m−2, while the head accumulated at the bottom of the fault scarp only represents 4.6 m3 m−2.
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https://hal.archives-ouvertes.fr/hal-00175551
Contributor : Marianne Font-Ertlen Connect in order to contact the contributor
Submitted on : Friday, September 28, 2007 - 3:39:34 PM
Last modification on : Monday, March 28, 2022 - 9:38:09 AM

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Marianne Font, J.L. Lagarde, D. Amorese, J.P. Coutard, J.C. Ozouf. Une méthode de quantification de la dégradation d'un escarpement de faille au cours des cycles climatiques du Quaternaire : la faille de Jobourg (Nord Cotentin, France).. Comptes Rendus Géoscience, 2002, 334 (3), pp.171-178. ⟨10.1016/S1631-0713(02)01732-7⟩. ⟨hal-00175551⟩

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