Thesis Collection
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Browsing by Subject "Betic Cordilleras"
Now showing items 1-20 of 22
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Características de la red de diques graníticos intruidos en las peridotitas de Ronda (Cordilleras Béticas)
(2006)This work analyses, from the structural point of view, the granite dyke swarm in the R onda area. Structural features of granite dykes from outcrop to microscopic scale show that their intrusion is controlled by ... -
Características petrográficas y mineralógicas de birbiritas derivadas de las peridotitas de Ronda (Cordilleras Béticas)
(Sociedad Geológica de España, 2011)Por primera vez en las Cordilleras Béticas describimos, en este trabajo, la existencia y las principales características mineralógicas y petrológicas de birbiritas que son el resultado de un intenso metasomatismo de ... -
Caracterización de la geometría del Polje de Zafarraya a partir de prospección gravimétrica (Cordillera Bética)
(Sociedad Geológica de España, 2016)The Zafarraya Polje is a Neogene endorheic basin, which lies on the contact between internal and external Zones of the Betic Cordillera. This basin limits on its southern boundary with the Ventas de Zafarraya fault, related ... -
Caracterización geoquímica y encuadre geodinámico de las anfibolitas y eclogitas del manto de Ojén, Complejo Alpujárride, Cordilleras Béticas
(Sociedad Geológica de España, 2009)Amphibolite bodies with eclogite relics are found interlayered between the Ojen nappe´s crustal rocks, below the Ronda peridotites of the Betic Cordilleras (southern Spain). We present a geochemical study of such ... -
Consideraciones sobre la edad del techo de las calizas oolíticas del Jurásico medio del Subbético Interno oriental (Cordilleras Béticas)
(Sociedad Geológica de España, 1996)Oolitic limestones crop extensively out in the External Zones of the Betic Cordilleras, currently being considered Dogger in age througt indirect criteria (mainly the age of the underlying and overlying units). In this ... -
El Sistema de Fallas Extensionales de La Axarquia (Sierras de Tejeda y La Almijara, Cordilleras Béticas)
Alonso Chaves, Francisco Manuel
; Orozco, Miguel (Sociedad Geológica de España, 1997)
The faults of La Axarquia Extensional System show a listric geometry. They cut across the uppermost alpujarride units and strongly contribute to the NW-SE mountain trend defined by the Tejeda-Almijara sierras. The main ... -
Estructura del Campo de Dalías a partir de datos gravimétricos y sísmicos
(Sociedad Geológica de España, 2004)The analysis of new gravity data and multichannel seismic profiles of the Campo de Dalías give new insight about the main features of the deep structure. The progressive development since the Tortonian of folds determine ... -
Estructura profunda del sector central de las Cordilleras Béticas
(Sociedad Geológica de España, 1994)The analysis of the crustal structure of the central sector of the Betic Cordilleras, by means of deep reflection seismic profiles and gravimetry, shows that the Moho is nearly planar. The continental crust of the Iberian ... -
Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
(Sociedad Geológica de España, 1992)The main deformation in the Tejeda and Canillas de Albaida Units is produced during a heterogeneous simple shearing regime that generates a planar-linear fabric. This simple shear has a topto-the-westsouhwest sense of ... -
Evolucìón petrogenética del magmatismo bàsico mesozoico en las Zonas Externas de las Cordilleras Béticas (S. España)
(Sociedad Geológica de España, 1996)Mesozoic basic magmatism from the External Zones of the Betic Cordilleras consisted of two magmatic events. The first one began at the end of the Triassic and the second developed during the Jurassic. Whole-rock geochemical ... -
Formación de grafito a partir de fluidos: La mineralización de Huelma (Jaén)
(Sociedad Geológica de España, 1996)The volcanic-hosted graphite mineralization of Huelma Qaén) has been studied in order to stablish the mineralogical characteristics and mechanisms of formation. The graphite is highly ordered (as revealed by XRD and Raman ... -
Generaciones de cabalgamientos y pliegues recumbentes en los Mantos Alpujárrides entre Ronda y Almería, Cordilleras Béticas
(Sociedad Geológica de España, 1987)Synmetamorphic thrust nappes, related to the Los Reales Crustal Thrust within the Alpujarride Nappes, moved in an ENE or NE direction. A subsequent movement took place in a northerly direction and large fold nappes were ... -
Origen de escapolitas asociadas a doleritas triásicas del Norte de la provincia de Cádiz
(Sociedad Geológica de España, 1996)Scapolites are present in some doleritic tectonic blocks C'ophites" )in the External Zones o f the Betic Cordilleras, In Northern of Cadiz province. These scapolites fill veinlets and replace plagioclases from the dolerites ... -
Primeros datos acerca de la evolución química de los Filosilicatos en el complejo Malaguide durante la fase Metamòrfica Alpina
(Sociedad Geológica de España, 1996)Compositional trends in the Maláguide Paleozoic, a very low-grade metamorphic complex of the Betlc Cordilleras, have been investigated in the Málaga area using bulk-rock mineralogy, clay mineralogy and chemical composition ... -
Relleno sedimentario y destrucción de una pequeña cuenca fluvio-lacustre en la Sierra Sur de Jaén (Cordilleras Béticas)
(Sociedad Geológica de España, 2002)The sedimentary infill of a small continental basin and the processes involved in its transformation into an erosionaI basin have been studied. The Otíñar basin is a fluvio-lacustrine basin developed during the Quaternary ... -
Rodingitización y formación de pectolita en diques graníticos de las Peridotitas de Ronda (Cordilleras Béticas, España)
(Sociedad Geológica de España, 2001)This work reports the local occurrence of rodingites formed from granitic dykes intrusive in the Ronda Peridotites. Representative mineral assemblages include chlorite, hydrogrossular, and prehnite but also pectolite, and ... -
El sentido de desplazamiento de los Mantos Nevado-Filábrides
(Sociedad Geológica de España, 1987)The Veleta Unit and the Mulhacen nappe Group (Calar Alto and Bédar-Macael Nap pes) make up the Nevado-Filábride Complex. The westward movement of the both nappes occurred along NW to WSW trajectories. In the Sierra Nevada, ... -
Superposición de estructuras corticales en la región de Archidona a partir de datos geofísicos (Zonas Externas de las Cordilleras Béticas)
(Sociedad Geológica de España, 1999)The region located at the NE of Archidona shows a maximum of aeromagnetic anomaly up to + 70 nT. This region, however, has minimum values of Bouguer anomaly (-120 mCal). New magnetic and gravimetric data and a P-wave seismic ... -
Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)
(Sociedad Geológica de España, 2003)This work reports the timing of the rodingitization process of granitic dykes intrusive into the Ronda Peridotites. Representative fission-track ages on zircon and apatite from rodingitized dykes, in combination with cooling ... -
Validez e interpretación de los datos geotermométricos de los esquistos cloríticos con circón en las peridotitas de Ronda (Cordilleras Béticas)
(2006)This work reports the most precise geochemical compositions and geothermometric calculations of zirconbearing chlorite schists located at the south-western part of the Sierra Bermeja peridotite massif. The combination ...
