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Resultats globals: 5 registres trobats en 0.02 segons.
Articles, 5 registres trobats
Articles 5 registres trobats  
1.
15 p, 3.6 MB Factors controlling the evolution of mineral assemblages and illite crystallinity in paleozoic to triassic sequences from the transition between maláguide and alpujárride complexes (betic cordillera, Spain) : The significance of tobelite / Ruiz Cruz, M. D. (Universidad de Málaga. Departamento de Química Inorgánica, Cristalografía y Mineralogía) ; Sanz de Galdeano, C. (Instituto Andaluz de Ciencias de la Tierra)
The Hercynian metamorphic event is poorly characterized in internal zone complexes of the Betic Cordillera (Spain), as it has been, to a great extent, overprinted by the mineral assemblages formed during the Alpine event. [...]
2010 - 10.1346/CCMN.2010.0580410
Clays and Clay Minerals, Vol. 58, Núm. 4 (2010) , p. 558-572  
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2.
49 p, 13.5 MB Glaucoceras gen. nov., a small uncoiled ammonoid from the Tethyan late Hauterivian (Early Cretaceous) : evolutionary implications at the dawn of the diversification of heteromorphic lineages / Matamales Andreu, Rafel (Institut Català de Paleontologia Miquel Crusafont) ; Juárez Ruiz, Josep (Societat d'Història Natural de les Balears) ; Pictet, Antoine (Musée Cantonal de Géologie) ; Moreno Bedmar, Josep Anton (Universidad Nacional Autónoma de México. Departamento de Paleontología) ; Universitat Autònoma de Barcelona
The poorly-known species Baculites Renevieri Ooster, 1860 is revised using the type material from Switzerland and new conspecific specimens collected in deposits from Mallorca and the Betic Cordillera (Western Mediterranean), listing all the previous mentions of the species. [...]
2019 - 10.1016/j.cretres.2019.02.025
Cretaceous research, Vol. 100 (August 2019) , p. 114-125  
Registre complet - Creative Commons
3.
16 p, 2.8 MB Late extensional shear zones and associated recumbent folds in the Alpujarride subduction complex, Betic Cordillera, southern Spain / Orozco Fernández, Miguel (Universidad de Granada. Departamento de Geodinámica) ; Alonso Chaves, Francisco Manuel (Universidad de Huelva. Departamento de Ciencias de la Tierra) ; Platt, J. P. (University of Southern California. Department of Earth Sciences)
The existence in the Alpujarride Complex (Betic Cordillera, southern Spain) of a relatively continuous extensional event (following crustal thickening) is based on detailed structural studies and is consistent with the P-T paths and geochronological data established for the Alpujarride rocks. [...]
2017 - 10.1344/GeologicaActa2017.15.1.5
Geologica acta, Vol. 15 Núm. 1 (march 2017) , p. 51-66 (Articles)  
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4.
20 p, 3.9 MB Organic-rich shales from internal Betic basins (SE Spain) : potential source rocks analogs for the pre-Messinian Salt play in the western Mediterranean / Permanyer Bastardas, Albert (Universitat de Barcelona. Departament de Geoquímica, Petrologia i Prospecció Geològica) ; Jorge, Robert (Universitat de Barcelona. Departament de Geoquímica, Petrologia i Prospecció Geològica) ; Baudino, Roger (Repsol Exploracion S.A) ; Gibert Beotas, Lluís (Universitat de Barcelona. Departament de Geoquímica, Petrologia i Prospecció Geològica)
Southeastern Spain has a large number of Late Neogene basins with substantial evaporitic deposits that developed under an overall NNW-SSE compressional regime related to the African-European tectonic plates collision. [...]
2014 - 10.1344/GeologicaActa2016.14.4.7
Geologica acta, Vol. 14 Núm. 4 (december 2016) , p. 443-460 (Special Issues: Selected contributions from the XIV ALAGO Congress)  
Registre complet - Creative Commons
5.
10 p, 1.1 MB From strike-slip to reverse reactivation : the Crevillente Fault System and seismicity in the Bullas-Mula area (Betic Cordillera, SE Spain) / Sanz de Galdeano, C. (Universidad de Granada. Facultad de Ciencias) ; Buforn, E. (Universidad Complutense de Madrid. Departamento de Geofísica y Meteorología) ; Consejo Superior de Investigaciones Científicas (Espanya). Instituto Andaluz de Ciencias de la Tierra
Several major N80ºE faults occur in the Bullas-Mula area (SE Spain). These faults and the numerous thrust slices of the Sierra de Ricote can be related to the movements of the Crevillente (or Cadiz-Alicante) fault system, which causes the westward displacement of the Betic Internal Zone and part of the External Zone. [...]
2005 - 10.1344/105.000001394
Geologica acta, Vol. 3, Núm. 3 (2005) , p. 241-250  
Registre complet - Creative Commons

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