Palaeomagnetic results from Upper Miocene and Pliocene rocks from the Internal Zone of the eastern Betic Cordilleras (southern Spain) [PDF]
Palaeomagnetic and rock-magnetic studies were carried out on samples from thirteen volcanic and nine sedimentary sites of Late Miocene to Pliocene age from the Internal Zone of the eastern Betic Cordilleras.
Calvo, Manuel +2 more
core +1 more source
Miocene extensional deformations in the region of Aguilas-Mazarrón (Eastern Betic Cordilleras) [PDF]
Some of the contacts between the superimposed tectonic units in the region of Aguilas-Mazarrón, in the Betic Zone, are normal low-angle faults. They are associated with ductile-fragile and fragile extensional structures, which, from the Lower Miocene ...
Aldaya, F. +2 more
core +3 more sources
Palaeogene to Early Miocene sedimentary history of the Sierra Espuña (Malaguide complex, internal zone of the Betic cordilleras, SE Spain). Evidence for extra-Malaguide (Sardinian?) provenance of oligocene conglomerates: Palaeogeographic implications [PDF]
The Sierra Espuña is situated at the northern edge of the Internal Zone in the eastern Betic Cordilleras and is part of the unmetamorphosed Malaguide Complex.
Geel, T.
core +3 more sources
Estromatolitos pelágicos fosfatados relacionados con discontinuidades estratigráficas en el Cretácico del Penibético (provincia de Málaga) [PDF]
En relación con discontinuidades estratigráficas en el Cretácico del Penibético se encuentran estromatolitos pelágicos fosfatados, constituidos por apatito criptocristalino (3 al 45 %).
García-Cervigón Bellón, Alfonso +3 more
core +1 more source
Tectónica reciente y activa en la parte occidental de la Cordillera Bética [PDF]
Based on new seismological and recent faulting data, we analyze five main sectors in the western part of the Betic Cordillera from an active tectonic perspective: i.
Galindo-Zaldivar, J. +4 more
core +2 more sources
Geochemistry and age relationships of metamorphosed mafic sills from Sierra de Enmedio and Sierra de Carrascoy (Eastern Betic zone, Southeastern Spain) [PDF]
The presence of fairly abundant shallow-intrusive mafic bodies is a common feature of the almagride units, a recently defined group of tectonic elements of the Eastern Betic Zone whose paleogeographic and tectonic interpretation is particuIarly ...
Puga, E., Torres-Roldán, R. L.
core +3 more sources
Application of Automated Throw Backstripping Method to Characterize Recent Faulting Activity Migration in the Al Hoceima Bay (Northeast Morocco): Geodynamic Implications [PDF]
This study was supported by projects CGL2016-80687-R AEI/FEDER, P18-RT-3275, B-RNM-301-UGR18 and RNM148 (Junta de Andalucia/FEDER); ALBAMAR JCJC ANR-17-CE030004; the EUROFLEETS program (FP7/2007-2013; no 228344); project FICTS-2011-03-01; and the FPU PhD
Tendero-Salmerón, Víctor +7 more
core +2 more sources
Volcaniclastites as a key for geodynamic constraints in the evolution of the central-western Mediterranean region: an overview [PDF]
In the central-western peri-Mediterranean chains, a consistent latest Chattian-Langhian orogenic calc-alkaline magmatism generated a high amount of volcaniclastites interbedded within penecontemporaneous marine successions.
Guerrera, Francesco +3 more
core +1 more source
El Torcal de Antequera, un ejemplo de estructura formada por un importante sistema transcurrente dextrorso [PDF]
The Torcal de Antequera is situated in the Penibetic (part of the Betic External Zone) very near of the contact with the Internal Zone. It has an E-W fusiform shape and corresponds to a monocline structure, surrounded and uplifted by large scale dextral ...
López Garrido, A. C. +1 more
core +3 more sources
Fracturación y control tectosedimentario neógeno en el borde sureste de la Cuenca de Lorca [PDF]
En este trabajo se estudia el control tectosedimentario ejercido por la fracturación neógena en la sedimentación en el borde suroriental de la Cuenca de Larca. El control más importante está impuesto por la actividad del Corredor Tectónico de la Falla de
Hernández Enrile, José Luis +1 more
core +1 more source

