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dc.contributor.authorSerra Kiel, Josep
dc.contributor.authorTravé i Herrero, Anna
dc.contributor.authorMató, E.
dc.contributor.authorSaula, E.
dc.contributor.authorFerràndez i Cañadell, Carles
dc.contributor.authorBusquets, Pere (Busquets i Buezo)
dc.contributor.authorTosquella Angrill, Josep 
dc.contributor.authorVergés i Masip, Jaume
dc.date.accessioned2014-01-23T09:29:16Z
dc.date.available2014-01-23T09:29:16Z
dc.date.issued2003
dc.identifier.citationSerra-Kiel, J., Travé i Herrero, , A., Mató, E., Saula, E., Ferràndez i Cañadell, C., Busquets, P., Tosquella Angrill, J., Vergés i Masip, J.: "Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)". Geologica Acta. Vol. 1, n. 2, págs. 177-200 (2003). ISSN 1695-6133
dc.identifier.issn1695-6133
dc.identifier.urihttp://hdl.handle.net/10272/7609
dc.description.abstractThe 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.en_US
dc.language.isoengen_US
dc.publisherInstitut de Ciències de la Terra "Jaume Almera"en_US
dc.publisherUniversidad de Barcelona
dc.publisherInstitut de Diagnosi Ambiental i Estudis de l'Aigua
dc.publisherUniversidad Autónoma de Barcelona
dc.publisherConsejo Superior de Investigaciones Científicas
dc.publisherInstitut Geològic de Catalunya
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherMarine unitsen_US
dc.subject.otherMiddle/Upper Eoceneen_US
dc.subject.otherLithostratigraphyen_US
dc.subject.otherBiostratigraphyen_US
dc.subject.otherPyrenean basin.en_US
dc.titleMarine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)en_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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