Sedimentación mixta (siliclásticoscarbonatada) en lagos someros de baja pendiente con dominio del oleaje. Un ejemplo del Mioceno de la Cuenca del Duero

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dc.book.titleLimmogeology in Spain: a tribute to Kerry R. Kelts
dc.contributor.authorMediavilla, Rosa
dc.contributor.authorSantisteban Navarro, Juan Ignacio
dc.contributor.authorDabrio González, Cristino José
dc.contributor.editorValero-Garcés, Blas L.
dc.date.accessioned2023-10-06T07:36:55Z
dc.date.available2023-10-06T07:36:55Z
dc.date.issued2003
dc.description.abstractLaeustrine deposits of Tecto-Sedimentary Unit N3 (Mediavilla et al., 1996) outcropping at the centcr of the Duero River Basin contain both, siliciclastic and carbonate formations. The siliciclastic formations were deposited in floodplain (oehre sands and muds), swamp (black and green muds) and lacustrine (green sands and muds) environments, and the carbonates (marls and massive, laminated, and cross-stratified limestones) are of Iacustrine origino Sequential analysis of these deposits reveals that both were coeval and formed in a single lakc. Their occurrence was a function of the distance of the sedimentation area to the siliciclastic sources. This model is ao altemative to their interpretation as an alternation of lithologieally different lakes. Therefore, the sedimentary sequenee can be interpreted as paleogeographically more than climatically controlled. This alternative interpretation urges for the use of correlations based on sequential analysis more than on Iithology for the study of sllch deposits.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.identifier.isbn84-00-08164-1
dc.identifier.urihttps://hdl.handle.net/20.500.14352/88165
dc.language.isospa
dc.page.final118
dc.page.initial99
dc.page.total440
dc.publication.placeMadrid
dc.publisherConsejo Superior de Investigaciones Científicas
dc.relation.ispartofseriesBiblioteca de ciencias, 14
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internationalen
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject.cdu551.3
dc.subject.keywordShallow lakes
dc.subject.keywordLow gradient lacustrine margin
dc.subject.keywordSiliciclastic-carbonated sediments
dc.subject.keywordNeogene
dc.subject.ucmGeología estratigráfica
dc.subject.unesco2506.18 Sedimentología
dc.titleSedimentación mixta (siliclásticoscarbonatada) en lagos someros de baja pendiente con dominio del oleaje. Un ejemplo del Mioceno de la Cuenca del Duero
dc.typebook part
dc.type.hasVersionVoR
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relation.isAuthorOfPublicationc83ed60c-056b-4da6-91a0-01121fce5299
relation.isAuthorOfPublication55faa814-a938-4b9e-9840-d51419e44f20
relation.isAuthorOfPublication.latestForDiscoveryc83ed60c-056b-4da6-91a0-01121fce5299
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