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Format
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Journal
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Section
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Angola (1)
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East Africa
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Tanzania (1)
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East African Rift (1)
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North Africa
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Algeria
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Atlas Mountains
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Moroccan Atlas Mountains
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Anti-Atlas (5)
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High Atlas (4)
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Egypt
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Sinai Egypt (2)
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Maghreb (1)
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Morocco
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Moroccan Atlas Mountains
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Rif
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Tunisia
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Nubia (1)
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Asia
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Oman
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Atlantic Ocean
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North Atlantic
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Russian Federation
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Orenburg Russian Federation (1)
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Russian Arctic
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Ukraine
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Orenburg Russian Federation (1)
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Greek Macedonia
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Iberian Peninsula
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Yeso Formation (1)
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Llandovery
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Wenlock
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Primary terms
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absolute age (76)
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Vermes (1)
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Vaca Muerta Formation (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
southwestern Iberian Peninsula
Wenlock–Ludlow graptolite biostratigraphy and extinction: a reassessment from the southwestern Iberian Peninsula (Spain and Portugal) Free
Stratigraphic Setting in the Development of Microbial Mud Mounds of the Lower Carboniferous of the Guadiato Area (Sw Spain) Available to Purchase
Abstract Sierra de la Estrella outcrops belong to the Sierra del Castillo Unit, which is defined in the Guadiato Area, SW Spain, where sedimentation occurred during the Late Viséan. The Guadiato Area is located on the boundary between the Ossa-Morena and Central Iberian structural zones, in the southwestern Iberian Peninsula, where Lower Carboniferous outcrops are common. The stratigraphic succession from Sierra de la Estrella is dated precisely by means of foraminifers (Zone 15). The studied rocks are interpreted as having developed on a storm-dominated ramp. Microbial buildups occur interbedded between tempestites and marls. Two main types of mud mounds have been distinguished: large tabular and smaller dome-shaped mud mounds, which were developed in a middle-ramp setting.
High-Resolution Seismic Stratigraphy of a Narrow, Bedrock-Controlled Estuary: The Guadiana Estuarine System, SW Iberia Available to Purchase
A new genus of nautiloid in the Toarcian of the Iberian peninsula (Spain and Portugal) Available to Purchase
NEW AND REVISED OCCURRENCES OF ORDOVICIAN CRINOIDS FROM SOUTHWESTERN EUROPE Available to Purchase
Small-mammal diversity in Spain during the late Pleistocene to early Holocene: Climate, landscape, and human impact Available to Purchase
Reconstructing a Super-Eruption From the Upper Ordovician Period in the Eastern Pyrenees, Spain Open Access
The Ordovician of France and neighbouring areas of Belgium and Germany Available to Purchase
Abstract The Ordovician successions of France and neighbouring areas of Belgium and Germany are reviewed and correlated based on international chronostratigraphic and regional biostratigraphic charts. The same three megasequences related to the rift, drift and docking of Avalonia with Baltica can be tracked in Belgium and neighbouring areas (Brabant Massif and Ardenne inliers), western (Rhenish Massif) and northeastern Germany (Rügen). The remaining investigated areas were part of Gondwana in the Ordovician. The Armorican Massif shares with the Iberian Peninsula a Furongian–Early Ordovician gap (Toledanian or Norman gap), and a continuous Mid–Late Ordovician shelf sedimentation. The Occitan Domain (Montagne Noire and Mouthoumet massifs), eastern Pyrenees and northwestern Corsica share with southwestern Sardinia continuous shelf sedimentation in the Early Ordovician, and a Mid Ordovician ‘Sardic gap’. In the Ordovician, the Maures Massif probably belonged to the same Sardo-Occitan domain. The Vosges and Schwarzwald massifs display comparable, poorly preserved Ordovician successions, suggesting affinities with the Teplá-Barrandian and/or Moldanubian zones of Central Europe.
( a ) Variscan tectonostratigraphic zones of the Iberian Peninsula highligh... Available to Purchase
Schematic map of the study area. A ) Map of the Iberian Peninsula and the ... Available to Purchase
New Middle Ordovician hyoliths from the Ossa Morena Zone, southwestern Spain Available to Purchase
Ranges and basins in the Iberian Peninsula: their contribution to the present topography Available to Purchase
Abstract The Iberian Peninsula, at the western end of the Alpine-Himalayan Belt, displays a complex structure with mountain ranges of diverse structural trends and sedimentary basins between them. The Iberian Peninsula also shows an elevated mean topography, the highest in Europe. In this short paper, we investigate the Alpine evolution of the Iberian Peninsula since Mesozoic times, when Iberia was isolated as an independent plate. This occurred from Albian (formation of the northern plate boundary) to Oligocene times (end of the Pyrenean Orogeny). Iberia was squeezed between Africa and Europe during Tertiary times and all previously established Mesozoic extensional basins were inverted, as were some of the Hercynian structures. The opening of the Valencia Trough, cutting the eastern margin of the Iberian Peninsula, began in Oligocene times. Concomitant crustal and lithospheric stretching during the Neogene along the eastern margin of Iberia produced limited uplifts, some of which are still active. The modern topography of the Iberian Peninsula was developed mainly as the result of three main tectonothermal mechanisms since late Palaeozoic times: variations in crustal densities, and possibly mantle depletion, inherited from the Hercynian Orogeny; crustal and lithospheric thickening during Tertiary compression; and upper mantle thinning during the Neogene-Quaternary.
Romain Vullo received his Licence degree in biology from the University of ... Available to Purchase
The Early Cretaceous of the Iberian Basin (Northeastern Spain) Available to Purchase
Abstract The Iberian Basin is an extensional intracratonic basin located in the northeastern part of the Iberian Peninsula (Figure 1). Sequence stratigraphy, subsidence analysis, and integration of basin fill data allow recognition of four successive evolutionary stages in the Iberian Basin during Mesozoic extension (Salasand Casas, 1993): (1) Triassic rift (Late Permian Hettangian);(2) Early and Middle Jurassic post-rift(Sinemurian-Oxfordian): (3) Late Jurassic-Early Cretaceousrift (Kimmeridgian-middle Albian); and (4)Late Cretaceous post-rift (late Albian-Maastrichtian).Evolution and formation of the Iberian Basin during the Mesozoic correlates well with the evolution of the North Atlantic marginal basins, the Aquitaine Basin, and the central south Pyrennean Basin (Tankard and Balkwill, 1989; Salas and Casas, 1993). The first two stages are related to the opening and spreading of the Neotethys toward the west. The third stage is related to the opening of the central Atlantic, and the fourth stage results from the opening of the Bay of Biscayaccompanied by the counterclockwise rotation of the Iberian plate and the consequent opening of the North Atlantic (Salas and Casas, 1993). During the Early Cretaceous, several isolated and well-differentiated subbasins formed in the IberianBasin. The origin of these subbasins is related to a riftingphase that took place during the Early Cretaceous concomitant with an increase in tectonic activity (Salas257and Casas, 1993; Salas et al., 1995), creating horsts,grabens, and half-grabens controlled by listric faults(Salas, 1983); moreover, reactivation of strike-slip basement faults, inherited from the late Hercynian, seemsto have controlled Cretaceous sedimentation (Salas and Casas, 1993). Infill of these small Early Cretaceous subbasins began with continental