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Baeza Carratalá, José Francisco ; Garcia Joral, Fernando | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2012The Lower Jurassic multicostate zeillerids of the Subbetic Domain are described here for the first time. A new species (Fimbriothyris? dubari) is erected, and the affinities of the remaining three species are discussed. These taxa appear as part[...]texto impreso
Dahlquist, Juan A. ; Pankhurst, R.J. ; Rapela, Carlos W. ; Galindo Francisco, Mª del Carmen ; Alasino, Pablo H. ; Fanning, C.M. ; Saavedra, Julio ; Baldo, Edgardo G. | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2008New SHRIMP U-Pb zircon ages are reported for igneous and sedimentary rocks of the Famatina Complex, constraining the age of the magmatism and the ensialic basins. Together with whole-rock and isotope geochemistry for the igneous rocks from the c[...]texto impreso
Duarte, Luís Vitor ; Silva, Ricardo ; Oliveira, Luiz Carlos Veiga de ; Comas Rengifo, María José ; Silva, Francisco | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2010The upper Sinemurian to Pliensbachian series of the Lusitanian Basin (Portugal) correspond to marly limestone sediments rich in benthic and nektonic macrofauna. This sedimentary record includes several intervals of organicrich facies, which are [...]texto impreso
Canora Catalán, Carolina ; Villamor Pérez, María Pilar ; Martínez Díaz, José J. ; Berryman, K.R. ; Álvarez Gómez, José Antonio ; Capote del Villar, Ramón ; Hernández, Walter | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2012The El Salvador earthquake of February 13th 2001 (Mw 6.6) was associated with the tectonic rupture of the El Salvador Fault Zone. Paleoseismic studies of the El Salvador Fault Zone undertaken after this earthquake provide a basis for examining t[...]texto impreso
Pérez-Soba Aguilar, Cecilia ; Villaseca González, Carlos | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2010The La Pedriza pluton stands out as the most extensively fractionated granite (Rbtexto impreso
Alonso-Zarza, Ana María ; Bones, B. | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2007The rugged karst terrain developed on the dolostones of the Miocene Cayman Formation (Fm) on Grand Cayman includes numerous large cavities that formed through the activity of tree roots. The surfaces of those cavities are coated with laminated c[...]texto impreso
Murra, Juan Alberto ; Baldo, Edgardo G. ; Galindo Francisco, Mª del Carmen ; Casquet, César ; Pankhurst, R.J. ; Rapela, Carlos W. ; Dahlquist, Juan A. | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2011The Sierra Brava Complex on the eastern flank of the Sierra de Ancasti consists of marbles, metabasites, calc-silicate rocks, psammo-pelitic schists and gneisses. In the central part of this sierra a thick succession of banded schists (Ancasti F[...]texto impreso
Arche, Alfredo ; López Gómez, José ; Marzo Carpio, Mariano ; Vargas, Henar | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2004The siliciclastic deposits of the Iberian, Ebro and Catalan Basins have been described for more than a century, but facies similarities and a lack of biostratigaphic data have difficulted the correlation of the local stratigraphic units in a gen[...]texto impreso
Liesa Torre Marín, Montserrat ; Carreras, Jordi ; Castiñeiras García, Pedro ; Casas Tuset, Josep María ; Navidad Fernández de la Cruz, Marina ; Vilà i Pranella, Miquel | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2011New geochronological data from the Albera Massif confirm the presence of an Early – Mid Ordovician igneous event (472 - 465Ma) recorded in the pre-Variscan rocks of the Pyrenees. This event resulted in the emplacement of a large granitic body in[...]
