Sequential and biostratigraphic correlations can be established in the lower Cretaceous of S.E. France. They provide evidence for a remarquable coincidence between : 1) the major sedimentological crises, which are especially perceptible on the perivocontian platforms ; 2) the tectonic crises ; and 3) the biological crises which affect the populations of the subalpine platform as well as those of the vocontian trough.Des corrélations séquentielles et biostratigraphiques détaillées sont possibles dans les assises éocrétacées du S.E. de la France. Elles montrent qu'il existe une coïncidence remarquable entre les crises sédimentologiques majeures, sensibles surtout sur les plates-formes périvocontiennes, les crises tectoniques et les crises bio...
On the northern flank of the Pyrénées, the appearance of continental facies, corresponding pro parte...
Abstract: Field observations suggest that prograding bioclastic wedges of depositional sequences in ...
International audienceContinental erosion and weathering destroy parts of the stratigraphic record. ...
Sequential and biostratigraphic correlations can be established in the lower Cretaceous of S.E. Fran...
International audienceA large area of synsedimentary collapse covering about 25 km2 has been identif...
Siliciclastic coastal series of the Rhone valley and thick calcareous basinal series of the Vocontia...
The detailed study of depositional geometries and facies of sedimentary successions from the Jura pl...
Siliciclastic coastal series of the Rhone valley and thick calcareous basinal series of the Vocontia...
Chronostratigraphically the middle Cretaceous is located at the transition from lower Cretaceous to ...
In South of Dôme de Barrot, the Cenomanian deposits display faciès of external platform. During Ceno...
International audienceSituée dans les Chaînes subalpines méridionales, la région du Dévoluy-Bochaine...
International audienceSituée dans les Chaînes subalpines méridionales, la région du Dévoluy-Bochaine...
The Upper Cretaceous sequence of Corsica is characterized by three main faciès : 1, a littoral facie...
On the northern flank of the Pyrénées, the appearance of continental facies, corresponding pro parte...
Abstract: Field observations suggest that prograding bioclastic wedges of depositional sequences in ...
International audienceContinental erosion and weathering destroy parts of the stratigraphic record. ...
Sequential and biostratigraphic correlations can be established in the lower Cretaceous of S.E. Fran...
International audienceA large area of synsedimentary collapse covering about 25 km2 has been identif...
Siliciclastic coastal series of the Rhone valley and thick calcareous basinal series of the Vocontia...
The detailed study of depositional geometries and facies of sedimentary successions from the Jura pl...
Siliciclastic coastal series of the Rhone valley and thick calcareous basinal series of the Vocontia...
Chronostratigraphically the middle Cretaceous is located at the transition from lower Cretaceous to ...
In South of Dôme de Barrot, the Cenomanian deposits display faciès of external platform. During Ceno...
International audienceSituée dans les Chaînes subalpines méridionales, la région du Dévoluy-Bochaine...
International audienceSituée dans les Chaînes subalpines méridionales, la région du Dévoluy-Bochaine...
The Upper Cretaceous sequence of Corsica is characterized by three main faciès : 1, a littoral facie...
On the northern flank of the Pyrénées, the appearance of continental facies, corresponding pro parte...
Abstract: Field observations suggest that prograding bioclastic wedges of depositional sequences in ...
International audienceContinental erosion and weathering destroy parts of the stratigraphic record. ...