http://www.cnr.it/ontology/cnr/individuo/prodotto/ID28514
Geomorphological, paleontological and 87Sr/86Sr isotope analyses of early Pleistocene paleoshorelines to define the uplift of Central Apennines (Italy) (Articolo in rivista)
- Type
- Label
- Geomorphological, paleontological and 87Sr/86Sr isotope analyses of early Pleistocene paleoshorelines to define the uplift of Central Apennines (Italy) (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.yqres.2007.01.005 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Marco Mancini; Elisabetta D'Anastasio; Mario Barbieri; Paolo Marco De Martini (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://www.journals.elsevier.com/quaternary-research/ (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Marco Mancini, Consiglio Nazionale delle Ricerche - Istituto di Geologia Ambientale e Geoingegneria;
Elisabetta D'Anastasio, Istituto Nazionale di Geofisica e Vulcanologia;
Mario Barbieri, Università degli Studi di Roma \"La Sapienza\" - Dipartimento di Scienze della Terra;
Paolo Marco De Martini, Istituto Nazionale di Geofisica e Vulcanologia (literal)
- Titolo
- Geomorphological, paleontological and 87Sr/86Sr isotope analyses of early Pleistocene paleoshorelines to define the uplift of Central Apennines (Italy) (literal)
- Abstract
- The eastern border of the Middle Valley of the Tiber River is characterized by several Plio-Pleistocene paleoshorelines, which extend for about
100 km along the western margin of the Central Apennines (Italy). We studied these paleoshorelines by the means of geological and
paleontological analyses and new 87Sr/86Sr isotope analyses. The youngest and uppermost paleoshorelines have been detected and mapped
through detailed geologic and stratigraphic surveys, which led to the recognition of nearshore deposits, cliff breccias, alignments of Lithophaga
borings, fossil abrasion notches and wave-cut platforms. The altitude of these paleoshorelines decreases almost regularly in the NNW-SSE
direction from 480 to 220 m a.s.l. Measurements of the 87Sr/86Sr isotope ratio have been conducted on corals and mollusks collected from
sediments outcropping close to the paleoshorelines. The isotopic dating results indicate numerical values that range between 0.70907 and 0.70910
all over the 100-km outcrop. These results, together with biostratigraphic data, constrain the age of the youngest paleoshorelines to 1.65-1.50 Ma.
These paleoshorelines are thus considered almost isochronous, giving an estimated uplift rate of 0.34-0.17±0.03 mm/a moving from NNW to
SSE. Shape, length and continuity of the 100-km-long observed movements indicate that the studied paleoshorelines are an important marker of
the Quaternary uplift of the Central Apennines. (literal)
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