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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Primary terms
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Africa
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Braux France
Rheological Complexity In Sediment Gravity Flows Forced To Decelerate Against A Confining Slope, Braux, SE France
D110 Braux Road section, Annot Sandstone, southeast France, illustrating tu...
Salt tectonics along a strike-slip fault system in the sub-Alpine chains of southeastern France, from the Triassic to the Oligocene
Migration of a synclinal depocentre from turbidite growth strata: the Annot syncline, SE France
Process Controls on the Development of Stratigraphic Trap Potential on the Margins of Confined Turbidite Systems and Aids to Reservoir Evaluation
—Map of the Maritime Alps in southeastern France showing in the inset the t...
The stratigraphic evolution of onlap in siliciclastic deep-water systems: Autogenic modulation of allogenic signals
REVIEWS
Delta-Fed Turbidites Infilling Topographically Complex Basins: A New Depositional Model for the Annot Sandstones, SE France
Simplified geological map of Southeast France showing the Tertiary outliers...
a) Synthetic structural map of the Annot syncline (key on fig. 3 ) showing ...
Linking Spatial Statistics to GIS: exploring potential gold and tin models of Africa
Deep-water sedimentation on an evolving fault-block: the Braux and St Benoit outcrops of the Grès d'Annot
Abstract The record of sediment fill contained in sub-basins of the western outcrops of the Grès d'Annot indicates that, throughout the period of deposition of the sandstones, there was very little synsedimentary tectonic activity. However, evidence of syntectonic sedimentation is preserved in the basal portion of the fill of the Annot sub-basin. The lowermost portions of the turbidite infill of the Annot sub-basin crop out around Braux and St Benoit. These outcrops are separated by the St Benoit Fault, which is thought to have developed as a result of sinistral strike-slip movement on the main Rouaine Fault to the south. The St Benoit Fault has a normal offset of up to 400 m to the east. Detailed mapping within the Calcaires Nummulitiques, Marnes Bleues and Grès d'Annot, has led to the recognition of several features that indicate a syntectonic sedimentary evolution for the outcrops. These record a three-phase progressive evolution of the St Benoit Fault through the upper Calcaires Nummulitiques to the lowermost Grès d'Annot. As part of this, there are implications for deposition from turbidity currents on encountering topographic barriers. To our knowledge, this area contains one of the few outcrop examples of half-graben formation within the confined basins of the Grès d'Annot.