A5021922990- Geological and Geophysical Studies Worldwide
- earthquake and tectonic studies
- Mediterranean and Iberian flora and fauna
- Geological formations and processes
- Infectious Diseases and Tuberculosis
- Hydrocarbon exploration and reservoir analysis
- Geological and Geochemical Analysis
- Hydrology and Sediment Transport Processes
- Therapeutic Uses of Natural Elements
- Geological and Tectonic Studies in Latin America
- Geology and Paleoclimatology Research
- Methane Hydrates and Related Phenomena
- African Studies and Geopolitics
- Water management and technologies
- Enhanced Oil Recovery Techniques
Université de Bordeaux
2012-2021
Institut Polytechnique de Bordeaux
2013-2021
The Atlas Mountains are classically regarded as a failed Mesozoic rift arm subject to Alpine inversion, folding and thrusting. Here, we present new integrated structural sedimentological studies that have revealed numerous Early–Middle Jurassic diapiric ridges minibasins, characterized by distinctive halokinetic structures. Diachroneity in halokinesis is observed across the Central High Atlas, waning first SW during (Jbel Azourki Tazoult ridges) continuing late Middle towards NE (Imilchil...
Research Article| July 01, 2012 New insights into the morphology and sedimentary processes along western slope of Great Bahama Bank T. Mulder; Mulder 1Université Bordeaux 1, UMR 5805 EPOC, 33405 Talence cedex, France Search for other works by this author on: GSW Google Scholar E. Ducassou; Ducassou G.P. Eberli; Eberli 2Division Marine Geology Geophysics, University Miami, Florida 33149, USA V. Hanquiez; Hanquiez Gonthier; Gonthier P. Kindler; Kindler 3Section Earth Environmental Sciences,...
The central High Atlas (Morocco) constitutes a diapiric province that hosts complex array of elongated diapirs and minibasins formed during the Lower Jurassic rift Basin. This paper aims to study structure growth evolution Tazoult wall, located in Atlas, by means structural sedimentological fieldwork integrated with remote sensing mapping. salt wall is 20 km long × 3 wide NE-SW trending ridge exposes Upper Triassic red beds basalts along its core. succession flanking ranges from Hettangian...
Abstract The subsidence evolution of the Tethyan Moroccan Atlas Basin, presently inverted as Central High Atlas, is characterized by an Early Jurassic rifting episode, synchronous with salt diapirism Triassic evaporite‐bearing rocks. Two contrasting regions rift basin – and without are examined to assess effect tectonics in patterns stratigraphy. Djebel Bou Dahar platform system, located southern margin shows a Lower record normal faulting lacks any evidence diapirism. In contrast, Tazoult...