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NARROW
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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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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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Europe
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Central Europe
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apatite (1)
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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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bibliography (2)
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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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folds (3)
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geophysical methods (5)
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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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Lower Cretaceous (1)
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Upper Cretaceous
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Campanian (1)
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Maestrichtian (1)
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Jurassic (1)
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Triassic
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Upper Triassic (1)
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metamorphic rocks
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eclogite (1)
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granulites (1)
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metamorphism (1)
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orogeny (10)
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paleogeography (1)
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Devonian
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Old Red Sandstone (1)
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petroleum
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natural gas (1)
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plate tectonics (11)
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sediments (1)
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South America
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Brazil (1)
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structural analysis (1)
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structural geology (1)
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tectonics
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salt tectonics (4)
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sedimentary rocks
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sedimentary rocks
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chemically precipitated rocks
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evaporites (1)
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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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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Revisiting orogens during the OROGEN project: tectonic maturity, a key element to understand orogenic variability Open Access
Grain-size analysis of the Late Pleistocene sediments in the Corinth Rift: insights into strait-influenced hydrodynamics and provenance of an active rift basin Available to Purchase
Abstract Grain-size analysis of the sediments in borehole M0079A, located in the Corinth Rift, was used to explore hydrodynamic conditions and provenance in the Late Pleistocene Corinth Rift. Grain-size populations that were sensitive to the sedimentary environments were characterized by frequency distribution, particle size–standard deviation and probability cumulative curves. Our results indicate the grain-size population component in the range 0.15–0.25 µm may be used as a sensitive proxy for hyperpycnal flows, which have commonly been triggered by river floods from the southern margin of the rift since c. 0.593–0.613 Ma. The high-density plumes derived from the longer rivers of the southern rift that were prevalent before c. 0.593–0.613 Ma. When sediment is supplied as hemipelagic deposition, the proportion of the total grain-size population that is in the 0.3–0.5 µm range becomes an index for suspension fall-out deposits. The core shows coarser sediments during the marine periods, and this may be linked to the current circulation related to the Ishtmia Strait opening. The study thus illustrates how the establishment of interbasinal straits can influence the details of sedimentary hydrodynamics in the deep-water axis of an adjacent depocentre.
Evolution of a low convergence collisional orogen: a review of Pyrenean orogenesis Open Access
Passive imaging of collisional orogens: a review of a decade of geophysical studies in the Pyrénées Open Access
Cenozoic mountain building and topographic evolution in Western Europe: impact of billions of years of lithosphere evolution and plate kinematics Open Access
The role of inheritance in forming rifts and rifted margins and building collisional orogens: a Biscay-Pyrenean perspective Open Access
Assessment of the tectonic role of the Triassic evaporites in the North Toulon fold-thrust belt Open Access
Geodynamic evolution of a wide plate boundary in the Western Mediterranean, near-field versus far-field interactions Open Access
Extension and early orogenic inversion along the basal detachment of a hyper-extended rifted margin: an example from the Central Pyrenees (France) Available to Purchase
Evidence of decoupled deformation during Jurassic rifting and Cenozoic inversion phases in the salt-rich Corbières-Languedoc Transfer Zone (Pyreneo-Provençal orogen, France) Open Access
A parametric fault displacement model to introduce kinematic control into modeling faults from sparse data Available to Purchase
Building up or out? Disparate sequence architectures along an active rift margin—Corinth rift, Greece Open Access
Erratum for ‘Retro-wedge foreland basin evolution along the ECORS line, eastern Pyrenees, France,’ Journal of the Geological Society , 173, 419–437 Free
Rift migration and lateral propagation: evolution of normal faults and sediment-routing systems of the western Corinth rift (Greece) Available to Purchase
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.
Retro-wedge foreland basin evolution along the ECORS line, eastern Pyrenees, France Available to Purchase
Impact of the en echelon fault connectivity on reservoir flow simulations Available to Purchase
Migration of a synclinal depocentre from turbidite growth strata: the Annot syncline, SE France Available to Purchase
Two-phase orogenic convergence in the external and internal SW Alps Available to Purchase
3D stratigraphic and structural synthesis of the Dannemarie basin (Upper Rhine Graben) Available to Purchase
Foreland basin evolution around the western Alpine Arc Available to Purchase
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.