Search results for "Cuencas continentales"

showing 2 items of 2 documents

Up-to-date Spanish continental Neogene synthesis and paleoclimatic interpretation

1993

A synthesis of the Spanish continental Neogene is presented by designing an integrated correlative chart of the Neo" gen-e "succes"Siuns-ofthe "lberian-PeninsuIa-. -Ninemain-sedimentary-breaks-have-been -distinguished-in-most-of-the "basins. They are considered a valuable criteria for correlation as they occur in similar time intervals from basin to basin. The determined sedimentary breaks occur in the Agenian, Ramblian, Middle Aragonian, Late Aragonian, Late Vallesian, Middle Turolian, Late Turolian, Late Ruscinian-Early Villafranchian, and Villafranchian ages. The larger interior basins (Ebro, Tajo, Duero) show a fairly complete Neogene sedimentary record in which the aboye mentioned sedi…

:CIENCIAS DE LA TIERRA Y DEL ESPACIO::Geología::Geología regional [UNESCO]UNESCO::CIENCIAS DE LA TIERRA Y DEL ESPACIO::Geología::Geología regionalPaleoclimasCuencas continentalesEspañaContinental basinsPaleoclimates SpainCorrelación estratigráficaStratigraphic correlation Sedimentary discontinuitiesNeógenoNeógeno; Cuencas continentales; Correlación estratigráfica; Discontinuidades sedimentarias; Paleoclimas; EspañaGeología estratigráficaNeogeneDiscontinuidades sedimentariasNeogene; Continental basins; Stratigraphic correlation Sedimentary discontinuities; Paleoclimates Spain
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The Ventian mammal age (Latest Miocene): present state

2013

[EN] The Ventian land mammal age includes most of the Spanish faunas assigned to the biochronologic unit MN 13. It is correlatable with the Messinian, although it may include, in its latest part, Early Pliocene faunas. We propose that the Ventian begins with the fi rst occurrence of the Muridae genus Stephanomys (7 Ma, paleomagnetic dating from El Bunker, Teruel basin), well recorded in Teruel basin, and ends with the appearance of Promimomys (ca. 5 Ma), also registered in the Teruel basin. We suggest a new reorganization of the Ventian. The first subdivision corresponds to the zone M (Dam et al., 2001). The second, zone N, is proposed here for the first time, being equivalent to the zone w…

PaleomagnetismCuencas continentalesMessiniensePaleontologyContinental basinsBiochronologyStructural basinPenínsula IbéricaArchaeologyQE701-760PaleontologyLa edad de mamíferos ventienses (Mioceno terminal): estado actualGeographyGenusMessinianestado actual [La edad de mamíferos ventienses (Mioceno terminal)]MammalBiocronologíabiochronology iberian peninsula continental bassin messinianIberian Peninsula
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