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Pleistocene evolution of the Seine river preserved in the Bay of Seine

Autor: Benabdellouahed , M., Dugué , O., Tessier , B., Thinon , I., Guennoc , P.

Publikováno v: Quaternaire
Quaternaire, AFEQ-CNF INQUA, 2013, 24 (3), pp.267-277. ⟨10.4000/quaternaire.6688⟩
Quaternaire, Centre National de la Recherche Scientifique, 2013, 24 (3), pp.267-277

International audience; New high-resolution seismic data complemented with bedrock samples allowed us to propose a revised geological map of the Bay of Seine and to better define the control by the geological substrate on the rphogenesis and evolutio

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::9068145287aed2b21502ec5a3c39062c
https://hal.archives-ouvertes.fr/hal-00997096

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Quaternary evolution of the Marrakech High Atlas and morphotectonic evidences of the Tizi N'Test Fault activity, Morocco

Autor: Delcaillau , B., Laville , E., Amhrar , M., Namous , M., Dugué , O., Pedoja , K.

Publikováno v: Geomorphology
Geomorphology, Elsevier, 2010, 118 (3-4), pp.262-279. ⟨10.1016/j.geomorph.2010.01.006⟩
Geomorphology, Elsevier, 2010, 118 (3-4), pp.262-279. 〈10.1016/j.geomorph.2010.01.006〉

International audience; Here, we consider the Ourika and Rheraia drainage basins on the Tizi NTest Fault zone in the mountains of the Marrakech High Atlas (western Morocco) with regard to Late Pleistocene tectonic activity. New insights into geomorph

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::ed05476229e3a7ed80a399a8f768b792
https://hal.archives-ouvertes.fr/hal-01002495

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The Cenozoic (Paleocene to lower Pleistocene) sedimentary evolution of the Normandy

Autor: Dugué , O., Lautridou , J.P., Quesnel , F., Clet , M., Poupinet , N., Bourdillon , C.

Publikováno v: Quaternaire
Quaternaire, AFEQ-CNF INQUA, 2009, 20 (3), pp.275-303
Quaternaire, Centre National de la Recherche Scientifique, 2009, 20 (3), pp.275-303

International audience; In the NW Normandy, only the Cotentin peninsula has preserved record of a thick Cenozoic sedimentary series (about 280 m) covered partially by Holocene sediments. As late as the Eocene, the Cotentin basin was open toward the A

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::4cdd9c0415aad4d8cf9b2b7976aa4e7c
https://hal.archives-ouvertes.fr/hal-00440260

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Les ammonites du Pliensbachien et du Toarcien basal dans la carrière de la Roche Blain (Fresnay-le-Puceux, Calvados, Basse-Normandie, France). Taxonomie, implications stratigraphiques et paléobiogéographiques

Autor: Dommergues , Jean-Louis, Dugué , O., Gauthier , H., Meister , Christian, Neige , Pascal, Raynaud , D., Savary , X., Trevisan , M.

Publikováno v: Revue de Paléobiologie
Revue de Paléobiologie, Museum d'Histoire Naturelle de la Ville de Geneve, 2008, 27 (1), pp.265-329

65 pages; International audience; Résumé Ce travail étudie les riches faunes d'ammonites du Pliensbachien et de la base du Toarcien dans la localité très fossilifère de la carrière de la Roche Blain (Calvados). Une cinquantaine d'espèces plie

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::bae1d75a48b8b85f80382baaceba001a
https://hal.archives-ouvertes.fr/hal-00325239

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Deciphering the origins of fine-grained deposits on the Calvados beaches (Normandy, France)

Autor: Dubrulle , C., Lesueur , P., Boust , D., Poupinet , N., Dugué , O., Lafite , R., Brun-Cottan , J.C.

Publikováno v: ECSA 38th Symposium : Changes in lands uses : consequences on estuaries and coastal zones
ECSA 38th Symposium : Changes in lands uses : consequences on estuaries and coastal zones, Sep 2004, Rouen, France

International audience

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::822baa822fff7e23af01d11f1c4aa44f
https://hal.archives-ouvertes.fr/hal-01455509

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The structural evolution of the English Channel area

Autor: Lagarde , J.L., Amorese , D., Font-Ertlen , M., Laville , E., Dugué , O.

Publikováno v: Journal of Quaternary Science
Journal of Quaternary Science, Wiley, 2003, 18 (3-4), pp.201-213. ⟨10.1002/jqs.744⟩
Journal of Quaternary Science, Wiley, 2003, 18 (3-4), pp.201-213. 〈10.1002/jqs.744〉

International audience; The structural evolution of the English Channel area is controlled by structure and particularly by the pre-existing Cadomian and Variscan crustal discontinuities, which have been reactivated repeatedly in post-Variscan times.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::af7334500a381412391a7806d2999cef
https://hal.archives-ouvertes.fr/hal-00175556

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