Zobrazeno 1 - 10
of 107
pro vyhledávání: '"Amédro , Francis"'
Publikováno v:
Comptes Rendus. Géoscience, Vol 354, Iss S3, Pp 67-87 (2022)
A tectonically-controlled forced regression occurred on the western margin of the French subalpine basin around the Aptian–Albian boundary. It nearly emptied the western part of the Vocontian Trough during the early and middle Albian. A compression
Externí odkaz:
https://doaj.org/article/ecf0e01cad424ea5aef6daccda65ada6
Autor:
Deconinck, Jean-François, Boué, Danny, Amédro, Francis, Baudin, François, Bruneau, Ludovic, Huret, Emilia, Landrein, Philippe, Moreau, Jean-David, Santoni, Anne Lise
Publikováno v:
In Cretaceous Research September 2021 125
Autor:
Corentin, Pauline, Deconinck, Jean-François, Pellenard, Pierre, Amédro, Francis, Bruneau, Ludovic, Chenot, Elise, Matrion, Bertrand, Huret, Emilia, Landrein, Philippe
Publikováno v:
In Cretaceous Research April 2020 108
Autor:
Bomou, Brahimsamba, Deconinck, Jean-François, Pucéat, Emmanuelle, Amédro, Francis, Joachimski, Michael M., Quillévéré, Frédéric
Publikováno v:
In Proceedings of the Geologists' Association December 2016 127(6):699-711
The Paris Basin is a Meso-Cenozoic intracontinental basin characterised during the Early Cretaceous by a continental evolution. However, in its southeastern part, due to transgressions originating from the Tethys, the Lower Cretaceous continental
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3711::ba4ee1383dd67644369b60c8dcc5742f
https://u-bourgogne.hal.science/hal-04065279
https://u-bourgogne.hal.science/hal-04065279
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
Amédro Francis
Publikováno v:
Carnets de Géologie, Vol CG2008, Iss M02, Pp 1-83 (2008)
The geological scale for the middle Cretaceous currently used throughout the world was proposed by Alcide d'Orbigny in the XIXth century between the years 1842 and 1847 and establishes the succession of stages as Albian, Cenomanian and Turonian. In 1
Externí odkaz:
https://doaj.org/article/4bcb1858b6fc4a829ce516f69dae1fa6
Autor:
Amédro Francis, Robaszynski Francis
Publikováno v:
Carnets de Géologie, Vol CG2008, Iss L02 (fr), Pp 6-10 (2008)
Depuis la fin du 19ème siècle, l'intervalle comprenant l'Albien supérieur élevé, le Cénomanien, le Turonien et le Coniacien basal a été subdivisé d'abord en zones d'ammonites puis, à partir du milieu du 20ème siècle, en zones de foraminif
Externí odkaz:
https://doaj.org/article/7f52769313dd41988f042fd2168e6e36