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The Guadiana river delta

dc.contributor.authorMorales, Juan A.
dc.contributor.authorGarel, Erwan
dc.date.accessioned2018-10-29T14:12:46Z
dc.date.available2018-10-29T14:12:46Z
dc.date.issued2019
dc.description.abstractThe Guadiana Estuary is a good example of rock bounded estuary which consists of a single narrow estuarine channel with a meandering morphology imposed by faults systems affecting the hard geology of the substrate. Only along the last kilometers of the estuarine channel, the valley opens when Cenozoic Guadalquivir Basin formations appear. In this area, the Guadiana develops a prograding coastal system constituted by successive sandy barriers separated by salt marshes which configure a wave dominated delta. This progradation is possible thanks an interaction of the coastal agents which enhanced the silting in addition to a good availability of sediments. This chapter explains an explanation of the dynamic functioning of the open coastal environment, so as the resulting facies model.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.1007/978-3-319-93169-2_24pt_PT
dc.identifier.isbn978-3-319-93168-5
dc.identifier.urihttp://hdl.handle.net/10400.1/10897
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherSpringerpt_PT
dc.subjectGuadiana estuarypt_PT
dc.titleThe Guadiana river deltapt_PT
dc.typebook part
dspace.entity.typePublication
oaire.citation.endPage581pt_PT
oaire.citation.startPage565pt_PT
oaire.citation.titleThe Spanish Coastal Systemspt_PT
person.familyNameGarel
person.givenNameErwan
person.identifier.ciencia-id5D13-7EA7-6C6D
person.identifier.orcid0000-0002-4584-9759
person.identifier.ridN-9811-2014
person.identifier.scopus-author-id23491739700
rcaap.rightsrestrictedAccesspt_PT
rcaap.typebookPartpt_PT
relation.isAuthorOfPublication7e619cba-3bfb-4964-bdf3-b8afd91a4a29
relation.isAuthorOfPublication.latestForDiscovery7e619cba-3bfb-4964-bdf3-b8afd91a4a29

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