Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Burdigalien"'
Autor:
Fauré, Philippe
We describe several new unconformable marine Miocene outcrops on the Lower Cretaceous of the Mediterranean coast of Saint-Martin Iceland (Gruissan, Aude). None had been identified to date. They are evidence of a maximum Neogene marine transgression o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______166::8bb8a54fd513581db40a0037b1bc6a79
https://hal.science/hal-03910300
https://hal.science/hal-03910300
Publikováno v:
Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
Universitat Autònoma de Barcelona
Altres ajuts: CERCA Programme/Generalitat de Catalunya Fossil turtles from Mokrá-Quarry, South Moravia Region, Czech Republic, are described in this paper. Remains come from two already known karstic fissures uncovered in Mokrá-Western Quarry (1/
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2e66fc9b92d65f16db8d62d51cc8226a
https://ddd.uab.cat/record/251228
https://ddd.uab.cat/record/251228
Autor:
Fauré, Philippe
We describe several examples of the marine Neogene transgression on the Lower Cretaceous from Saint- Martin Island (Gruissan, Aude). Little was known of the composition of the Miocene there. Molassic limestones with Chlamys tournali of Burdigalian ag
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______166::da5eae9c79004d833f54ff55f0da8433
https://hal.archives-ouvertes.fr/hal-03762753
https://hal.archives-ouvertes.fr/hal-03762753
Publikováno v:
Geodiversitas
Geodiversitas, 2015, 37 (3), pp.367-381. ⟨10.5252/g2015n3a5⟩
Geodiversitas, 2015, 37 (3), pp.367-381. ⟨10.5252/g2015n3a5⟩
In Upper Burdigalian time, coral reefs developed within the Cala di Labra Formation, in the Bonifacio area (South Corsica, France). They are organized into three successive coral reef episodes R1, R2 and R3. The coral fauna comprising 16 reefal speci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2417::3f5b9f3f0dea97fd9883456a7b9f0c7f
https://hal.science/hal-01236095/document
https://hal.science/hal-01236095/document
Publikováno v:
Géologie de la France
Géologie de la France, BRGM, 2014, pp.47-66
Géologie de la France, 2014, pp.47-66
Géologie de la France, BRGM, 2014, pp.47-66
Géologie de la France, 2014, pp.47-66
National audience; À Bonifacio, la Formation de Cala di Labra renferme des constructions coralliennes constituant les témoins uniques d’une activité récifale hermatypique au Miocène inférieur en Corse. Leur édification durant la transgressio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::4ffafaa450d2297b65123e93109a283c
https://hal.archives-ouvertes.fr/hal-01690863
https://hal.archives-ouvertes.fr/hal-01690863
Autor:
J.F. Cubells, Jean Gaudant, Jean Ferrandini, Michelle Maurel-Ferrandini, Marie-Dominique Loÿe-Pilot
Publikováno v:
Géologie Méditerranéenne. 21:19-24
Among the four Corsican Miocene sedimentary basins, the Francardo-Ponte Leccia basin is the only one lying in the centre of the island. With a North-South axis, it is located at the frontier between the Hercynian and the Alpine parts of Corsica. The
Publikováno v:
Géologie Méditerranéenne. 21:69-83
Large scale eustatic events can be expected to influence marine sedimentation, not only in stable foreland settings but also in tectonically active regions. The signal characterizing each event is unique and can be recognized with confidence in all a
Autor:
Bauer, Hugues
Le besoin de connaître toujours plus finement les réservoirs (pétrole/gaz, stockage du CO2, des déchets...) se heurte au problème de la résolution temporelle (stratigraphique), notamment pour les séries sédimentaires continentales. Leur géom
Autor:
HUGUES BAUER
Publikováno v:
Sciences of the Universe [physics]. École Nationale Supérieure des Mines de Paris, 2006. English
HAL
HAL
The detailed study of reservoir (oil/gas, CO2 and waste storage...) architecture is first a stratigraphic challenge, more specifically for continental series. The geometry of such deposits is under the influence of three main factors: sea-level chang
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a723341b1cab195a98dde618325cd398
https://pastel.archives-ouvertes.fr/pastel-00002113/document
https://pastel.archives-ouvertes.fr/pastel-00002113/document