Arquitectura estratigráfica de la Fm. Escucha (Albiense) en el flanco sur del Sinclinal de Cueva Foradada. Subcuenca de Oliete (Teruel), Cuenca Ibérica Central

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dc.contributor.authorRodríguez López, Juan Pedro
dc.contributor.authorMeléndez Hevia, Nieves
dc.contributor.authorSoria, Ana Rosa
dc.date.accessioned2023-06-20T12:48:21Z
dc.date.available2023-06-20T12:48:21Z
dc.date.issued2005
dc.description.abstractDetailed stratigraphic sections have allowed to establish the stratigraphic architecture of the Escucha Formation in the southern limb of the asymmetrical Cueva Foradada Syncline (Oiete Subbasin, Iberian Basin, Spain). The stratigraphic correlation builded from the studied stratigraphic sections shows the spatial distribution of the main architectural elements and their spatial relationships. Offshore, intertidal, supratidal, flood delta / tidal inlet and bay-lagoon with tidal meandering channel facies associations occurred in a strongly tidal-influenced stratigraphic succession. The occurrence of several key stratigraphic levels characterized by the presence of nodular-iron rich levels with gastropods, levels of oyster accumulations and galuconitic sandstones suggest that the beginning of the Escucha Formation's evolution was characterized by the development of several transgressive periods that interrupted the development of coal-forming and tidal-influenced siliciclastic sedimentary subenvironments.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipSecretaría de Estado de Educación y Universidades
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/61364
dc.identifier.issn1576-5172
dc.identifier.officialurlhttp://www.sociedadgeologica.es/publicaciones_geotemas.html
dc.identifier.urihttps://hdl.handle.net/20.500.14352/52565
dc.journal.titleGeotemas
dc.language.isospa
dc.page.final98
dc.page.initial95
dc.publisherSociedad Geológica de España.
dc.relation.projectIDBTE 2002 - 04453 - C02 - 02.
dc.rights.accessRightsopen access
dc.subject.cdu551.7
dc.subject.keywordStratigraphic architecture
dc.subject.keywordTidal subenvironments
dc.subject.keywordTidal channels
dc.subject.keywordCoals
dc.subject.ucmGeología estratigráfica
dc.subject.unesco2506.19 Estratigrafía
dc.titleArquitectura estratigráfica de la Fm. Escucha (Albiense) en el flanco sur del Sinclinal de Cueva Foradada. Subcuenca de Oliete (Teruel), Cuenca Ibérica Central
dc.typejournal article
dc.volume.number8
dspace.entity.typePublication
relation.isAuthorOfPublication86a02762-7c9f-4535-b728-7ee0fdcefce3
relation.isAuthorOfPublication.latestForDiscovery86a02762-7c9f-4535-b728-7ee0fdcefce3
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