Thesis Collection
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Browsing by Author "Salas, Ramón"
Now showing items 1-14 of 14
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Ciclicidad de alta frecuencia en la megasecuencia sinrift titónico-berriasiense. Cuenca Ibérica oriental
(Sociedad Geológica de España, 1996)In the Iberian basin, the Tithonian-Berriasian supersequence (ZB-1 2 nd order supercycle) was deposited in a subsident regime during the moderate to intense rifting stages of the Jurassic phase. The repetitive character ... -
Ciclicidad de alta frecuencia en la megasecuencia sinrift titónicoberriasiense. Cuenca Ibérica oriental
(Sociedad Geológica de España, 1996)In the Iberian basin, the Tithonian-Berriasian supersequence (ZB-1 2 nd order supercycle) was deposited in a subsident regime during the moderate to intense rifting stages of the Jurassic phase. The repetitive character o ... -
Dolomías controladas por fracturas en carbonatos aptienses de la zona de Benicàssim (SE Cuenca del Maestrat): distribución y características petrograficas
(Universidad de Huelva, 2012)El estudio de dolomías se ha incrementado notablemente en la última década debido a la existencia de numerosos almacenes de petróleo en esta litología. Esta contribución presenta un nuevo ejemplo de dolomías controladas por ... -
El magmatismo alcalino jurásico del sector SE de la Cadena Ibérica: composición y estructura
(Sociedad Geológica de España, 1996)Jurassic volcanic rocks are well exposed in the Sierra de Javalambre (Teruel)., This multiepisodic volcanism is mainly volcaniclastic , showing a large variety of fragmentation and emplacement mechanisms, and it is ... -
Extensión mesozoica e inversión compresiva terciaria en la Cadena Ibérica: aportaciones a partir del análisis de un perfil gravimétrico
(Sociedad Geológica de España, 1996)The eastern part of Iberia underwent extension during the Mesozoic and, as a result, intraplate basins were formed. These basins were inverted during the Tertiary giving rise to the Iberian Chain thrust belt. The analysis ... -
Factores principales de control de la sedimentación y los cambios bióticos durante el tránsito Jurásico-Cretácico en la Cadena Ibérica
(Sociedad Geológica de España, 2005)The Iberian Chain developed by inversion of Mesozoic rifts of the Iberian Basin during the Paleogene. The Maestrat and Cameros basins developed during the Late Jurassic-Early Cretaceous rifting cycle 2. There are two ... -
Heavy mineral composition and geochemistry of the Weald facies from the Maestrat Basin (Spain): Provenance implications for Late Jurassic-Early Cretaceous rifting stage
(Sociedad Geológica de España, 2005)Las areniscas en facies Weald de la Cuenca del Maestrazgo fueron depositadas durante la etapa de rift Jurásico superior-Cretácico inferior. Una característica de las cuencas intracratónicas desarrolladas durante periodos ... -
Inversión terciaria de la falla normal mesozoica que limitaba la subcuenca de Calve (cuenca del Maestrazgo)
(Sociedad Geológica de España, 1996)An example of a Mesozoic normal fault with in the Maestrat basin is studied. This, fault dips to the South and bound two sub-basins; the Aliaga sub-basin, on the uplifted fault foot-wall, contains 320 m of syn-rift ... -
La Formación Arcillas de Morella (Aptiense Inferior), Cadena Ibérica oriental (España): caracterización sedimentológica
(Sociedad Geológica de España, 2003)The detail stratigraphy, sedlmentology and paleontology of the Arcillas de Morella Formation allows us to better understand the sedimentary environment in the northwestern part of the Maestrazgo Basin during the Lower ... -
La plataforma carbonatada Aptiense superior de Benicàssim-Orpesa (Cuenca del Maestrat, Cadena Ibérica): modelo de depósito
(2006)A Lower Cretaceous (Upper Aptian) succesion of carbonate rocks in the southwestern Maestrat Basin (Iberian Chain) was analysed according to sedimentological and palaeontological criteria. The shallow marine sequence was ... -
Las facies evaporíticas y carbonatadas del tránsito Triásico-Jurásico (Morata de Jalón, Zaragoza): relación tectónica-sedimentación
(2006)Facies analysis and geological mapping of the Triassic-Jurassic transition units (Cor tes de Tajuña and Lécera Fms) exposed in an area of 10 km2 around Morata de Jalón locality (Zaragoza province, North Iberian Range) ... -
Materia orgánica y diagénesis de la formación de margas del Mas d'Ascla (Jurásico superior) en la cuenca del Maestrazgo (Cadena Ibérica oriental)
(Sociedad Geológica de España, 1999)The Mas d'Ascla marls Fm. (Upper Kimmeridgian to lowermost Tithonian) in the Maestrat Basin (Salzedella sub-basin, Castellò de la Plana) displays two organic-carbon-rich horizons which indicate anoxic conditions. The maximum ... -
Precisiones sobre la edad, mediante ammonoideos y nautiloideos, de la Fm. Margas del Forcall en la subcuenca de Oliete (Cadena Ibérica, España)
(2007)Ammonoids and nautiloids from Margas del Forcall Formation, located in the Oliete sub-basin (Iberian Chain), were studied. Taphonomic, sedimentologic and biostratigraphic analyses were carried out. The fossil record of ... -
Rasgos estructurales principales de la cuenca cretácica inferior del Maestrazgo (Cordillera Ibérica oriental)
(Sociedad Geológica de España, 1996)The Maestrat basin (up to 6.5 km of Mesozoic sediments) is an intracontinental basin located in the Iberian Range (Iberian Basin), which underwent two significant rift stages during the Late Jurassic and Early Cretaceous. ...
