Utilize este identificador para referenciar este registo: http://hdl.handle.net/10362/4707
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dc.contributor.authorAntunes, M. Telles-
dc.contributor.authorLegoinha, P.-
dc.contributor.authorCunha, Pedro Proença-
dc.contributor.authorPais, João-
dc.date.accessioned2010-12-28T23:00:41Z-
dc.date.available2010-12-28T23:00:41Z-
dc.date.issued2010-12-28-
dc.identifier.urihttp://hdl.handle.net/10362/4707-
dc.description.abstractCorrelation between facies associations (marine, estuarine and distal fluviatile environments) and disconformities, observed between Foz da Fonte (SW of Setúbal Peninsula) and Santa Iria da Azóia (NE of Lisbon) are presented. The precise definition of the marine-continental facies relationships improved very much the chronology of the depositional sequence boundaries. Tectonic and eustatic controls are discussed on the basis of subsidence rates variation.en_US
dc.language.isoengen_US
dc.rightsopenAccessen_US
dc.subjectsequencial stratigraphyen_US
dc.subjectMioceneen_US
dc.subjectLower Tagus Basinen_US
dc.subjectLisbonen_US
dc.subjectSetúbal Peninsulaen_US
dc.subjectPortugalen_US
dc.titleHigh resolution stratigraphy and miocene facies correlation in Lisbon and Setúbal Peninsula (Lower Tagus basin, Portugal)en_US
dc.typearticleen_US
my.embargo.termsnullen_US
Aparece nas colecções:FCT: DCT - Ciências da Terra

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