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Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/16893

Title: Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)
Authors: Serra-Kiel, Josep
Travé i Herrero, Anna
Mató, E.
Saula, E.
Ferràndez i Cañadell, Carles
Busquets, Pere (Busquets i Buezo)
Tosquella i Angrill, Josep
Vergés i Masip, Jaume
Matèria: Conques sedimentàries
Litoestratigrafia
Bioestratigrafia
Eocè
Pirineus
Sedimentary basins
Lithostratigraphy
Biostratigraphy
Eocene Epoch
Pyrenean basin
Issue Date: 2003
Publisher: Universitat de Barcelona (UB). Institut de Ciències de la Terra Jaume Almera (ICTJA). Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDEA). Universitat Autonònoma de Barcelona (UAB). Consejo Superior de Investigaciones Científicas (CSIC)
Abstract: The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigraphic characterisation of the new Shallow Benthic Zones (SBZ). This part of the volume presents a description of the sedimentary cycles formed by the transgressive-regressive systems of the Lutetian and Bartonian in the southeastern sector of the Ebro Foreland Basin. Concerning the Lutetian deposits studied in the Amer-Vic and Empordà areas, four sedimentary cycles have been characterised. The first and second are found within the Tavertet/Girona Limestone Formation (Reguant, 1967; Pallí, 1972), while the third and fourth cycles cover the Coll de Malla Marl Formation (Clavell et al., 1970), the Bracons Formation (Gich, 1969, 1972), the Banyoles Marl Formation (Almela and Ríos, 1943), and the Bellmunt Formation (Gich, 1969, 1972). In the Bartonian deposits studied in the Igualada area, two transgressive-regressive sedimentary cycles have been characterised in the Collbàs Formation (Ferrer, 1971), the Igualada Formation (Ferrer, 1971), and the Tossa Formation (Ferrer, 1971). The Shallow Benthic Zones (SBZs) recognised within the Lutetian are the following: SBZ 13, from the Early Lutetian, in the transgressive system of the first cycle; SBZ 14, from the Middle Lutetian, in the second cycle and the lower part of the transgressive system of the third cycle; SBZ 15, from the Middle Lutetian, in the remaining parts of the third system; SBZ 16, from the Late Lutetian, throughout the fourth cycle. The association of larger foraminifers in the first and second cycles of the Bartonian in the Igualada area has been used as the basis for the definition of SBZs 17 and 18 recognised in the Bartonian of the western Tethys.
Nota: Reproducció del document publicat a http://www.geologica-acta.com/pdf/vol0102a07.pdf
És part de: Geologica Acta, 2003, vol. 1, núm. 2, p. 177-200
URI: http://hdl.handle.net/2445/16893
ISSN: 1695-6133
Appears in Collections:Articles publicats en revistes (Geoquímica, Petrologia i Prospecció Geològica)
Articles publicats en revistes (Estratigrafia, Paleontologia i Geociències Marines)

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