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Carracedo, Juan Carlos ; Ancochea Soto, Eumenio ; Pérez Torrado, Francisco José ; Meco, Joaquín ; Hernán, Francisco ; Cubas, Carmen Rosa ; Casillas, Ramón ; Rodríguez Badiola, Eduardo ; Ahijado, Agustina | Geological Society of London | 2002The Canarian archipelago comprises seven main volcanic islands and several islets that form a chain extending for c. 500 km across the eastern Atlantic, with its eastern edge only 100 km from the NW African coast. The islands have had a very lon[...]texto impreso
Villaseca González, Carlos ; Ancochea Soto, Eumenio ; Orejana García, David ; Jeffries, Teresa E. | Geological Society of London | 2010Spinel lherzolite xenoliths from the Cenozoic Calatrava volcanic field provide a sampling of the lithospheric mantle of central Spain. The xenoliths are estimated to originate from depths of 35–50 km. Trace element content of clinopyroxene and C[...]texto impreso
Fort González, Rafael ; Álvarez de Buergo, Mónica ; Pérez-Monserrat, Elena Mercedes ; Gómez Heras, Miguel ; Varas Muriel, María José | Geological Society of London | 2013Many types of stone have been used for construction in Madrid. In historical times, their use was determined by the proximity of the geological resources, the ease of quarrying and transportation links to the city. More recently, as transport co[...]texto impreso
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Díaz Molina, Margarita ; Arribas Mocoroa, José ; Gómez Fernández, Juan José ; Tortosa, A. | Geological Society of London | 1995The reconstruction of meander belts was approached by detailed geological mapping, the interpretation of exposed sandstone bodies and the application of sedimentological concepts. The single reconstructed meander belts were integrated, consideri[...]texto impreso
The alkaline lamprophyres and diabases from the Spanish Central System carry a heterogeneous suite of xenoliths including a group of highly altered ultramafic pyroxenites that contain Cr–Mg-rich high-T hydrous minerals (Ti-phlogopite and pargasi[...]texto impreso
Natural gamma spectral (NGS) log motifs and cluster analysis were used to characterize outcropping sandstone bodies formed in braided and highsinuosity streams of the Tertiary Tórtola fluvial system of the Loranca Basin (Spain). Five coarse-grai[...]texto impreso
Palaeogene detrital deposits of the northern Tajo Basin are coalescent alluvial fan systems interfingering distally with lacustrine carbonates. Non-carbonate extrabasinal clasts increase to the east while carbonate extrabasinal clasts decrease. [...]texto impreso
Tortosa, Amparo ; Arribas Mocoroa, José ; Palomares Herranz, Marta | Geological Society of London | 1991Holocene sands of the Spanish Central System were exclusively derived from plutonic , middle-upper grade and low-grade metamorphic rocks. Modal composition of studied sands is mostly controlled by grain size and source area lithology . Thus, san[...]texto impreso
Pérez López, Raúl ; Rodríguez-Pascua, M.A. ; Giner Robles, Jorge L. ; Martínez Díaz, José J. ; Marcos Nuez, A. ; Silva Barroso, Pablo Gabriel ; Bejar Pizarro, Marta ; Calvo Sorando, José Pedro | Geological Society of London | 2009-01-01This work describes the coseismic ceiling block collapse within Benis Cave (?213 m; Murcia, SE Spain), associated with the 1999 Mula earthquake (mb=4.8, MSK VII). The collapse occurred at ?156 m into the Earthquake Hall, and as a consequence one[...]texto impreso
Fernández Marrón, María Teresa ; López Martínez, Nieves ; Fonollá Ocete, José Fernando ; Valle-Hernández, M.F | Geological Society of London | 2004North American and Pacific spore-pollen records show a major extinction event at the Cretaceous Tertiary (K-T) boundary, and abrupt changes are similarly found in many marine organisms world-wide. In contrast, records from the Old World reveal l[...]
