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Autor Chacón Pichaco, Beatriz |
Documentos disponibles escritos por este autor (7)
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Martín Chivelet, Javier ; Chacón Pichaco, Beatriz ; Fregenal Martínez, María Antonia | Sociedad Geológica de España. | 2001This paper focuses on the deep marine carbonates of late Campanian to lower Maastricht!an age that crop out in the Subbetic Zone near Caravaca (Murcia province). Their sedimentological analysis allows to recognize a thick succession of dm-scale [...]texto impreso
In the upper Santonian to Danian hemipelagic to pelagic series in the eastern part o f the Prebetic Jumilla-Callosa-Aspe area, detailed stratigraphic and biostratigraphic analyses have allowed the recognition and age-dating of three major region[...]texto impreso
In the Eastern Prebetic Zone of SE Spain, upper Cretaceous to lower Eocene hemipelagic sequences deposited in the ancient southern passive continental margin of Iberia are well exposed. The long-term stratigraphy of these sequences is punctuated[...]texto impreso
En este trabajo se analizan depósitos de edad Santoniense a Eoceno inferior de gran parte de la provincia de Alicante y dos sectores de la región de Murcia. Está enmarcada en las Zonas Externas de la Cordillera Bética (parte oriental-meridional [...]texto impreso
This paper presents the first detailed biostratigraphic analysis of the uppermost Santonian through uppermost Maastrichtian hemipelagic carbonate successions of south-east Spain based mainly on the stratigraphic distributions of planktic foramin[...]texto impreso
Martín Chivelet, Javier ; Fregenal Martínez, María Antonia ; Chacón Pichaco, Beatriz | Elsevier | 2003Deep marine carbonates of Late Campanian to Early Maastrichtian age that crop out in the Subbetic Zone near Caravaca (SE Spain) contain a thick succession of dm-scale levels of calcareous contourites, alternating with fine-grained pelagites/ hem[...]texto impreso
The hemipelagic domain of the ancient southern continental margin of Iberia is home to a strongly condensed pelagic succession (6–15 cm thick) characterized by the presence of phosphate stromatolites. This succession, probably generated in the s[...]