Thesis Collection
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Browsing by Author "Vilas, Lorenzo"
Now showing items 1-6 of 6
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El Cretácico superior de la Sierra de las Moratillas (Prebético externo. Murcia)
(Sociedad Geológica de España, 1988)Nine litostratigraphic units are described in late Cretaceous of Sierra de las Moratillas (Murcia, Prebetic zone). Most of them find their equivalent inside Southern Iberian Ranges, others show little differences and just ... -
El Valanginiense superior de la sección de Oliva (Zona Prebética, Valencia): análisis de facies, bioestratigrafía, isótopos de carbono y geoquímica orgánica
(Sociedad Geológica de España, 2014)The Upper Valanginian stratigraphic section of the sierra de la Oliva (Prebetic, Valencia province) records a significant sedimentary episode which has been named as ”Weissert Event”.This event is characterized by a ... -
Episodios sedimentarios en el Alcudiense Superior (Proterozoico) y su tránsito al Cámbrico en la zona centro meridional del Macizo Ibérico
(Sociedad Geológica de España, 1987)The evolution of the Upper Alcudian-Lower Cambrian basin is studied in the eastern Lusitanian-Alcudian Zone. Five sedimentary episodes with distinctive characteristics are considered -
Estructuración del basamento mesozoico en Los Llanos de Albacete
(Sociedad Geológica de España, 1987)The Mesozoic basement of Los Llanos de Albacete Tertiary Basin shows a fracture grid with two main orientations, almost orthogonal: NE-SW orientation is preferential, causing the basement to be divided in several blocks, ... -
El límite meridional de la transgresión cenomaniense superior en la Cordillera Ibérica (Murcia, Albacete y Valencia)
(Sociedad Geológica de España, 1988)During Late Cenomanian, an Atlantic transgression occurs as a result of the Iberian Plate tilting. Its southern limit is recognized in the Murcia-Albacete-Valencia area, with continental sediments, which are dividing the ... -
Relaciones tectónica-sedimentación en el Aptiense de Sierra Larga, Jumilla (Murcia)
(Sociedad Geológica de España, 1996)Aptian shallow water carbonates of the Sierra Larga antiform (Prebetic of Murcia) show rapid vertical and lateral facies and thickness variations with well defined sequences. Each sequence consists of a lower terrigenous ...
