Thesis Collection
Last Deposit
Browsing by Author "Serrano Lozano, Francisco"
Now showing items 1-12 of 12
-
Caracterización de la sedimentación Lago Mare (Messiniense terminal) y de la transgresión del comienzo del Plioceno en la cuenca de Málaga (Cordillera Bética)
(2008)A stratigraphic unit deposited close to the Messinian-Pliocene boundary is newly discovered in the Malaga basin. This unit mainly consist of alluvial and lagoonal deposits. Paleontological and paleomagnetic data from ... -
Descubrimiento del Burdigaliense (formación Viñuela) en la cobertera Gomáride de Ceuta (Rif septentrional)
(Sociedad Geológica de España, 1999)In the Ceuta area, located at the northernmost end of the Rifian Internal Zones, new outcrops of the Tertiary Formations covering Chomarid units, are studied. The new data obtained allow to characterize the Fnidek Formation ... -
The early Pliocene Tirinesse basin (SW of Oued Laou, Rif, Morocco): proposal of a formation model
(Sociedad Geológica de España, 2014)The Tirinesse basin, filled mainly by lower Pliocene marine sediments, is a small tectonic graben bounded by two NE-SW normal faults, with the eastern one surpassing 500 m in throw. These faults proved to belong to a ... -
Estudio de los minerales de la arcilla en sedimentos del Messiniense terminal-Zancliense inferior en la cuenca de Málaga (S España). Resultados preliminares
(Universidad de Huelva, 2012)El análisis de la composición mineralógica global de los sedimentos Lago-Mare y del Zancliense inferior de la cuenca de Málaga muestra diferencias significativas hacia la mitad de la secuencia del Zancliense inferior. Este ... -
La serie paleógena de la unidad superior del Gomáride en Talembote (Rif Interno, Marruecos)
(2007)The lower Paleogene stratigraphic successions of the Talembote upper Ghomaride Unit represent an interval of age going from the (middle?) Ilerdian to the early Bartonian, showing a transgressive sequence interrupted by ... -
Las formaciones del mapa geológico a escala 1:25.000 de la Cuenca de Lorca (Murcia)
(Sociedad Geológica de España, 1996)The Lorca Basin is located in the Betic Ranges (SE o f Spain) over the contact between the Betic domain s.s. (in te rn a l zones) and the Subbetic one (external zones). For the complementary use of the mineralogical and ... -
Nuevos datos estratigráficos de la Unidad Central, Hauz Intermedio (Dorsal Rifeña). Consecuencias paleogeográficas
(Sociedad Geológica de España, 1994)The presence both of radiolarites, attributed to the Dogger-Malm, and grey marls from the early Late Eocene in the Intermediate U n it o f the Haouz M ountains (Rifian Dorsal) indicates that the sea occupied the area at ... -
Palaeoceanographer, una herramienta informática para estimar características paleoceanográficas de las aguas marinas superficiales del Cuaternario y Neógeno superior
(2008)This work presents Palaeoceanographer as a new computer tool that we designed for palaeoceanographic studies. However, the software utility can be also extended to other scientific areas in which the aim is to carry out ... -
Presencia de Serravalliense marino en la cuenca de Níjar (Cordillera Bética, España)
(Sociedad Geológica de España, 1989)The existence of marine sedimentary materials of the Middle Miocene in the Níjar Basin is noted. The series is extended from the Upper Langhian to Upper Serravallian. These materials were deposited in marine basin open to ... -
Subsidence and uplift during the Plio-Quaternary in the Oued Laou and Tirinesse sectors (Internal Rif, Morocco)
(Sociedad Geológica de España, 2014)The Oued Laou area and the Tirinesse basin are filled with early Pliocene (Zanclean) marine sediments very slightly deformed but currently outcropping at different altitudes. In Tirinesse area Zanclean sediments reach ... -
Tectónica sinsedimentaria en el Plioceno de Malalyine (NE de Tetuán, Rif, Marruecos)
(Universidad de Huelva, 2011)En el área de Malalyine, sedimentos pliocenos de un nuevo afloramiento están afectados por varios juegos de diaclasas compatibles con una compresión NW-SE y, particularmente, con una tensión perpendicular en dirección ... -
El Terciario de la unidad de Saaden ("Dorsal" externa, Rif Septentrional, Marruecos)
(Sociedad Geológica de España, 1993)In the Saaden unit (External "Limestone Chain", northern Internal Rif), the uppermost Eocene and the Oligocene have been dated by planktonic foraminifera. It confirms that an important transgression accounted during the ...
