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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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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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Europe
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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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Rif (1)
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West African Craton (1)
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Atlantic Ocean
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North Atlantic
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Bay of Biscay (1)
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South Atlantic
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bibliography (2)
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Quaternary
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crust (3)
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deformation (5)
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Europe
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Alps
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Piedmont Alps
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Dora Maira Massif (1)
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Western Alps
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Cottian Alps
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Dora Maira Massif (1)
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Central Europe
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Upper Rhine Graben (1)
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Pyrenees
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French Pyrenees (2)
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Southern Europe
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Greece (2)
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Iberian Peninsula
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Spain
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Betic Cordillera (1)
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Ebro Basin (1)
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Italy
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Piemonte Italy
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Dora Maira Massif (1)
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Variscides (1)
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Western Europe
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Cottian Alps
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Dora Maira Massif (1)
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France
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Aquitaine Basin (3)
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Ariege France (1)
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Aude France
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Corbieres (1)
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Brittany (1)
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faults (9)
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igneous rocks
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plutonic rocks
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ultramafics
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peridotites
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lherzolite (1)
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isostasy (1)
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mantle (3)
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Mediterranean region (3)
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Mediterranean Sea
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East Mediterranean
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Ionian Sea
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Gulf of Corinth (2)
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West Mediterranean
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Alboran Sea (1)
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Gulf of Lion (1)
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Tyrrhenian Sea (1)
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Mesozoic
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Cretaceous
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Jurassic (1)
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metamorphic rocks
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orogeny (9)
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sedimentary rocks
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sedimentary rocks
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turbidite (1)
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sediments
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sediments (1)
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turbidite (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
Assessment of the tectonic role of the Triassic evaporites in the North Toulon fold-thrust belt
Geodynamic evolution of a wide plate boundary in the Western Mediterranean, near-field versus far-field interactions
Extension and early orogenic inversion along the basal detachment of a hyper-extended rifted margin: an example from the Central Pyrenees (France)
Evidence of decoupled deformation during Jurassic rifting and Cenozoic inversion phases in the salt-rich Corbières-Languedoc Transfer Zone (Pyreneo-Provençal orogen, France)
A parametric fault displacement model to introduce kinematic control into modeling faults from sparse data
Building up or out? Disparate sequence architectures along an active rift margin—Corinth rift, Greece
Abstract: The active Corinth rift records hanging-wall migration of faulting and slip-rate acceleration. The rift initiated at approximately 5–4 Ma, and older parts are well exposed in the northern Peloponnese. A new correlation of chrono- and lithostratigraphy and structure across the onland central to westernmost rift with offshore data reveals westward rift propagation, as well as northward fault migration. Northward fault migration ended first in the east, with the stabilization of major north-dipping faults that now bound the Gulf. The basin then propagated to the WNW in two stages, each involving the initiation of a new fault that propagated east to SE to link to the stable fault system. Extension rates accelerated in distinct steps as the rift opened to the west. The youngest faults in the westernmost rift are associated with high seismicity and highest geodetic extension due to rapid fault growth and linkage at depth. The early synrift succession infilled substantial inherited palaeo-relief. Antecedent rivers established vigorous sediment-routing systems that controlled facies distribution throughout rifting, albeit with drainage reorganization during fault-migration events. Multiple deepening events recorded in the stratigraphy can be due to lateral rift propagation. The transition from rift initiation to rift climax is, therefore, diachronous along the rift axis.
Erratum for ‘Retro-wedge foreland basin evolution along the ECORS line, eastern Pyrenees, France,’ Journal of the Geological Society , 173, 419–437
Retro-wedge foreland basin evolution along the ECORS line, eastern Pyrenees, France
Impact of the en echelon fault connectivity on reservoir flow simulations
Migration of a synclinal depocentre from turbidite growth strata: the Annot syncline, SE France
Two-phase orogenic convergence in the external and internal SW Alps
3D stratigraphic and structural synthesis of the Dannemarie basin (Upper Rhine Graben)
Abstract The arcuate form of the external western Alps was generated during Tertiary NW-directed collision between the Apulian indentor and the southward-subducting European passive margin. The evolution of peripheral syn-collisional depocentres around this arcuate orogen (in France and Switzerland) is reconstructed using a compilation of stratigraphic and tectonic data. This reveals fundamental changes in the flexural behaviour of the European lithosphere during collision. During early collision (Eocene), an increasingly arcuate, peripheral flexural basin migrated rapidly NW across the European plate. During peak collision (early Oligocene), frontal flexure, recorded in the North Alpine Foreland Basin (NAFB), steepened markedly, while lateral flexure of the European plate, affecting SE France, effectively ceased. Here, Oligocene sedimentation was confined to small thrust-sheet-top basins. Two rift systems initiating in the late Eocene, the West European rift system and the West Mediterranean oceanic basin (that created the Gulf of Lion passive margin), are superimposed in space and time on the outer margins of the alpine flexural depocentres. During waning collision (Mio-Pliocene) the NAFB became overfilled, then uplifted and abandoned while, in SE France, a local depocentre (Digne-Valensole) developed between uplifting blocks and continued to accumulate sediments until the late Pliocene.