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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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Atlas Mountains
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Primary terms
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Morocco
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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bibliography (2)
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Spain
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Cantabrian Basin (1)
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Cantabrian Mountains (1)
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Evolution of a low convergence collisional orogen: a review of Pyrenean orogenesis
Passive imaging of collisional orogens: a review of a decade of geophysical studies in the Pyrénées
Cenozoic mountain building and topographic evolution in Western Europe: impact of billions of years of lithosphere evolution and plate kinematics
The role of inheritance in forming rifts and rifted margins and building collisional orogens: a Biscay-Pyrenean perspective
The North Pyrenean Frontal Thrust: structure, timing and late fluid circulation inferred from seismic and thermal-geochemical analyses of well data
Geodynamic evolution of a wide plate boundary in the Western Mediterranean, near-field versus far-field interactions
Distribution and intensity of High-Temperature Low-Pressure metamorphism across the Pyrenean-Cantabrian belt: constraints on the thermal record of the pre-orogenic hyperextension rifting
Post-orogenic exhumation in the western Pyrenees: evidence for extension driven by pre-orogenic inheritance
Abstract The Côte de l’Âne section has been previously interpreted as shallow marine deposits (deltaic system with delta-front to bay head and back-barrier environments). The purpose of this article is (1) to suggest a reinterpretation of these facies of the Grès d'Annot in this area as deep marine deposits and (2) to discuss the effect of an evolving seafloor topography during sedimentation on the stacking pattern of turbiditic deposits. The facies analysis of the sedimentary succession is based on eight measured sedimentological logs and on the visual correlation of identified surfaces. Detailed sedimentological observations permitted the identification of a turbidite facies spectrum, schematized in nine facies associations. Outcrop-scale analysis highlights a downstream thickening of the sedimentary sequence resulting from a strong control by tectonic deformation. This deformation is mainly a flexure with a half-wavelength longer than 500m. Associated normal faults may be related to a gravity slide of unconsolidated sediments accommodated within the flexure. Finally, detailed correlations based on the genetic unit model in the Restefonds-Sanguinière system establish the effect of an evolving seafloor topography during sedimentation on the stacking pattern of turbiditic deposits.