Results 251 to 260 of about 165,337 (293)
Assessment of Viticultural Biodiversity: Recovery of Indigenous Grapevine Genotypes from Ancient Vineyards of El-Kantara (<i>Calceus Herculis</i>) in Algeria. [PDF]
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Lithos, 2019
Voluminous peraluminous (biotite, biotite–cordierite and cordierite–muscovite-bearing) granitic plutons were emplaced in the southern part of the Central Iberian Zone (Iberian Massif) during the waning stages of the Variscan Orogeny.
Jon Errandonea-Martin +1 more
exaly +2 more sources
Voluminous peraluminous (biotite, biotite–cordierite and cordierite–muscovite-bearing) granitic plutons were emplaced in the southern part of the Central Iberian Zone (Iberian Massif) during the waning stages of the Variscan Orogeny.
Jon Errandonea-Martin +1 more
exaly +2 more sources
SGEM International Multidisciplinary Scientific GeoConference� EXPO Proceedings, 2023
In the Central Iberian Zone, multiple subvolcanic intrusions were emplaced during the final stages of the Variscan orogeny. The felsic component of this magmatic episode is mainly represented by dykes and masses of granite porphyries and microgranites ...
A. Oliveira +2 more
semanticscholar +2 more sources
In the Central Iberian Zone, multiple subvolcanic intrusions were emplaced during the final stages of the Variscan orogeny. The felsic component of this magmatic episode is mainly represented by dykes and masses of granite porphyries and microgranites ...
A. Oliveira +2 more
semanticscholar +2 more sources
Geochemistry, geochronology and mineralisation potential of the granites in the Central Iberian Zone: The Jalama batholith [PDF]
The Jalama batholith (Spain and Portugal) is one of the numerous granites ofthe Central Iberian Zone with Sn- and W-associated mineralisation. On the basis of petrographical and geochemical characterisation three types of granite have been distinguished: inhomogeneous granitoids, porphyrytic granites and leucogranites, all of these being
Concepción Fernández-Leyva
exaly +3 more sources
Caradoc through Early AshgillBrachiopods from the Central-Iberian zone (Central Spain)
Geobios, 1995Abstract Caradoc through early Ashgill brachiopods from the Central-Iberian Zone, representing the latest cold water brachiopodassociations of the West European Platform developed on the North-African Gondwana margin, have been studied. Twenty one brachiopod taxa, including two new species ( Tafilaltia brevimusculosa and Hedstroemina almadenensis ),
Enrique Villas
exaly +2 more sources
Journal of the Geological Society, 2022
The Figueira de Castelo Rodrigo – Lumbrales Anatectic Complex (FCR-LAC) located in the Central Iberian Zone of the European Variscan Belt is delimited by two shear zones, which have been interpreted as constraining its exhumation.
J. Ferreira +3 more
semanticscholar +1 more source
The Figueira de Castelo Rodrigo – Lumbrales Anatectic Complex (FCR-LAC) located in the Central Iberian Zone of the European Variscan Belt is delimited by two shear zones, which have been interpreted as constraining its exhumation.
J. Ferreira +3 more
semanticscholar +1 more source
Ordovician tectonics and crustal evolution at the Gondwana margin (Central Iberian Zone)
Journal of the Geological Society, 2022U-Pb ages of zircon from samples of tonalite and migmatite from the Central Iberian Zone (Spain), previously assigned to the Carboniferous were obtained using a sensitive high mass-resolution ion microprobe.
M. F. Pereira +3 more
semanticscholar +1 more source
Tectonophysics, 2001
Abstract We have investigated the stratigraphy, structure and metamorphism of the boundary between the Ossa Morena Zone (OMZ) and the Central Iberian Zone (CIZ), two significant continental portions of the Variscan Iberian Massif. The OMZ/CIZ contact is marked by a strongly deformed and metamorphosed NW–SE trending narrow band, namely, the Central ...
David Martinez Poyatos +2 more
exaly +2 more sources
Abstract We have investigated the stratigraphy, structure and metamorphism of the boundary between the Ossa Morena Zone (OMZ) and the Central Iberian Zone (CIZ), two significant continental portions of the Variscan Iberian Massif. The OMZ/CIZ contact is marked by a strongly deformed and metamorphosed NW–SE trending narrow band, namely, the Central ...
David Martinez Poyatos +2 more
exaly +2 more sources

