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| Campo DC | Valor | Lengua/Idioma |
|---|---|---|
| dc.provenance | Comisión de Investigaciones Científicas | - |
| dc.contributor | Zanchetta, Giovanni | - |
| dc.contributor | Bini, Mónica | - |
| dc.contributor | Isola, Ilaria | - |
| dc.contributor | Pappalardo, Marta | - |
| dc.contributor | Ribolini, Adriano | - |
| dc.contributor | Consoloni, Ilaria | - |
| dc.contributor | Boretto, Gabriella | - |
| dc.contributor | Fucks, Enrique | - |
| dc.contributor | Ragaini, Luca | - |
| dc.contributor | Terrasi, Filippo | - |
| dc.creator | Zanchetta, Giovanni | - |
| dc.creator | Bini, Mónica | - |
| dc.creator | Isola, Ilaria | - |
| dc.creator | Pappalardo, Marta | - |
| dc.creator | Ribolini, Adriano | - |
| dc.creator | Consoloni, Ilaria | - |
| dc.creator | Boretto, Gabriella | - |
| dc.creator | Fucks, Enrique | - |
| dc.creator | Ragaini, Luca | - |
| dc.creator | Terrasi, Filippo | - |
| dc.date | 2014-01-29 | - |
| dc.date.accessioned | 2019-04-29T16:06:02Z | - |
| dc.date.available | 2019-04-29T16:06:02Z | - |
| dc.date.issued | 2014-01-29 | - |
| dc.identifier | http://digital.cic.gba.gob.ar/handle/11746/5958 | - |
| dc.identifier | Recurso Completo | - |
| dc.identifier.uri | http://rodna.bn.gov.ar:8080/jspui/handle/bnmm/309176 | - |
| dc.description | Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Province, Argentina) indicate that the Holocene coastline formed in response to the discontinuous aggradation of coarse gravely beaches since<em>c.</em>6300 cal. yr BP related to a progressive falling of relative sea level. Beach ridge crests crudely approximate to the sea level showing at least three steps of aggradation and relative sea-level lowering. Two inactive abrasive notches at<em>c.</em>7.9 and 3.4 m a.s.l. have recorded this sea-level trend, suggesting two important phases when sea level was stationary. This allows the estimation of a rate of relative sea-level fall in the last<em>c.</em>3500 years of<em>c.</em>1.8 mm/yr. Moreover, notches and morphological data indicate that the crest of the beach ridges exceeded the sea-level height by<em>c.</em>2 ± 0.5 m. This value provides a reasonable regional estimate to be applied to produce comparable relative sea-level curve for Atlantic Patagonia coast. | - |
| dc.format | application/pdf | - |
| dc.format | 11 p. | - |
| dc.language | eng | - |
| dc.rights | info:eu-repo/semantics/openAccess | - |
| dc.rights | Attribution 4.0 International (BY 4.0) | - |
| dc.source | reponame:CIC Digital (CICBA) | - |
| dc.source | instname:Comisión de Investigaciones Científicas de la Provincia de Buenos Aires | - |
| dc.source | instacron:CICBA | - |
| dc.source.uri | http://digital.cic.gba.gob.ar/handle/11746/5958 | - |
| dc.source.uri | Recurso Completo | - |
| dc.subject | Geología | - |
| dc.title | Middle-to late-Holocene relative sea-level changes at Puerto Deseado (Patagonia, Argentina) | - |
| dc.type | info:eu-repo/semantics/article | - |
| dc.type | info:eu-repo/semantics/submittedVersion | - |
| dc.type | info:ar-repo/semantics/articulo | - |
| Aparece en las colecciones: | Comisión de Investigaciones Científicas de la Prov. de Buenos Aires | |
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