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The postglacial sea level rise within the Guadiana Estuary- a contribution to a regional record in the Gulf of Cadiz

dc.contributor.authorBoski, T.
dc.contributor.authorMoura, Delminda
dc.contributor.authorLourenço, Nuno
dc.contributor.authorVeiga-Pires, C.
dc.date.accessioned2013-03-21T10:42:59Z
dc.date.available2013-03-21T10:42:59Z
dc.date.issued2000
dc.description.abstractIn the Guadiana River Estuary, the Holocene estuarine infill is underlain by coarse delta fan sediments enclosing saltmarh deposits, dating back to isotope stage 5e or a stage 3 interstadial highstands.por
dc.identifier.otherAUT: DMO00293;
dc.identifier.urihttp://hdl.handle.net/10400.1/2618
dc.language.isoengpor
dc.peerreviewedyespor
dc.publisherEnrique Schnack & Colin Murray-Wallacepor
dc.subjectSealevel risepor
dc.subjectGuadiana Estuarypor
dc.subjectPostglacialpor
dc.subjectGulf of Cadizpor
dc.titleThe postglacial sea level rise within the Guadiana Estuary- a contribution to a regional record in the Gulf of Cadizpor
dc.typeconference object
dspace.entity.typePublication
oaire.citation.conferencePlacePuerto Madryn- Argentinapor
oaire.citation.endPage18por
oaire.citation.startPage15por
oaire.citation.titleCoastal Interactions during sea-level highstandspor
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person.familyNameLourenço
person.familyNameVeiga-Pires
person.givenNameTomasz
person.givenNameDelminda
person.givenNameNuno
person.givenNameCristina
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person.identifier.ridA-5361-2013
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person.identifier.scopus-author-id6602267486
person.identifier.scopus-author-id15048413000
person.identifier.scopus-author-id57216555279
person.identifier.scopus-author-id7801372905
rcaap.rightsopenAccesspor
rcaap.typeconferenceObjectpor
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