Thesis Collection
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Browsing by Subject "Iberian basin"
Now showing items 1-7 of 7
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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 ... -
Control tectónico y distribución de las facies en el tránsito Triásico-Jurásico en el sector de Oliete (Teruel)
(Sociedad Geológica de España, 1998)Facies and thickness distribution in the Cortes de Tajuña Fm. was controlled by extensional fault activity around the Triassic-Jurassic boundary in the Iberian basin. The analysis of the outcrops located South of Oliete ... -
Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)
(Sociedad Geológica de España, 1997)Facies distribution and sedimentary procceses in a storm dominated carbonate ramp (Kimmeridgian, northern Iberian basin) is studied in detail. Shallow ramp areas are dominated by coral reef facies. They grade basinsward ... -
El Bathoniense-Kimmeridgiense (Jurásico medio-superior) en la región de Obón-Torre de las Arcas (Teruel)
(Sociedad Geológica de España, 1998)The middle-upper Jurassic of the Obón-Torre de las Arcas area (Teruel province, northern Iberian Chain) consists of five stratigraphic units. Unit I is formed by oolitic grainstones (c. 20 m thick) and was developed during ... -
La discordancia de Moyuela (Zaragoza): precisiones sobre la tectónica extensional en el límite Oxfordiense-Kimmeridgiense en la Cuenca Ibérica
(Sociedad Geológica de España, 1997)An angular unconformity has been found at the lower part of the Sot de Chera Fm. near the village of Moyuela (Northern Iberian Chain, NE Spain). This unconformity develops during a tectonic extension at the turn of the ... -
Origen de las brechas de la base del Jurásico en Morata de Jalón (Zaragoza)
(Sociedad Geológica de España, 1996)A sedimentary breccia is found in the lower Liassic (Hettangian?) in wide areas of the Iberian Chain (NE Spain). This breccia was originated during a tectonic extension at the onset of the Jurassic by a number of procceses, ...
