Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2044
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dc.contributor.authorallAiello, G.; Dip. Sc. della Terra, Università di Napolien
dc.contributor.authorallAscione, A.; Dip. Sc. della Terra, Università di Napolien
dc.contributor.authorallBarra, D.; Dip. Sc. della Terra, Università di Napolien
dc.contributor.authorallMunno, R.; Dip. Sc. della Terra, Università di Napolien
dc.contributor.authorallPetrosino, P.; Dip. Sc. della Terra, Università di Napolien
dc.contributor.authorallRusso Ermolli, E.; Dip. Sc. della Terra, Università di Napolien
dc.contributor.authorallVillani, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2007-02-08T10:01:03Zen
dc.date.available2007-02-08T10:01:03Zen
dc.date.issued2006en
dc.identifier.urihttp://hdl.handle.net/2122/2044en
dc.description.abstractThe Pantano di San Gregorio Magno is a 4.7 km 2 large tectono-karstic basin located in the axial belt of the Southern Apennines, an area affected by intense seismicity. The basin was formed in the Middle Pleistocene and is presently undissected. It is filled by lacustrine sediments (clays, silts and pyroclastic sands) passing laterally into alluvial fan deposits. Geomorphological investigations were integrated with tephrostratigraphical, palynological and palaeoecological analyses of a 61 m thick core (not reaching the bedrock). The multiproxy analysis of the S. Gregorio Magno record shows that, over the last 200k yr, the basin hosted a freshwater lake with an oscillating level. Age constraints provided by the tephrostratigraphic record allowed estimation of the sedimentation rate, which varied strongly through time. Evolution of the basin resulted from the complex combination of tectonic subsidence, karst processes and changing amounts of sedimentary inputs. The latter was influenced by allogenic contributions related both to primary and reworked volcanoclastic inputs and was climate-driven. The overall evidence, which indicates that in the long-term the accumulation rate substantially counterbalanced the accommodation space created by faulting, suggests that the basin evolution was also modulated by changing subsidence rates.en
dc.format.extent555688 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameWiley Interscienceen
dc.relation.ispartofJournal of Quaternary Scienceen
dc.subjectSouthern Apenninesen
dc.subjectlate Quaternaryen
dc.subjectgeomorphologyen
dc.subjecttephrostratigraphyen
dc.subjectpalaeoenvironmentsen
dc.titleEvolution of the late Quaternary San Gregorio Magno tectono-karstic basin (southern Italy) inferred from geomorphological, tephrostratigraphical and palaecological analyses: tectonic implicationsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.03. Geomorphologyen
dc.identifier.doi10.1002/jqs.1040en
dc.description.fulltextreserveden
dc.contributor.authorAiello, G.en
dc.contributor.authorAscione, A.en
dc.contributor.authorBarra, D.en
dc.contributor.authorMunno, R.en
dc.contributor.authorPetrosino, P.en
dc.contributor.authorRusso Ermolli, E.en
dc.contributor.authorVillani, F.en
dc.contributor.departmentDip. Sc. della Terra, Università di Napolien
dc.contributor.departmentDip. Sc. della Terra, Università di Napolien
dc.contributor.departmentDip. Sc. della Terra, Università di Napolien
dc.contributor.departmentDip. Sc. della Terra, Università di Napolien
dc.contributor.departmentDip. Sc. della Terra, Università di Napolien
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità degli Studi di Napoli "Federico II", Dipartimento di Scienze della terra, Largo S. Marcellino 10, 80138 Napoli-
crisitem.author.deptUniversità di Napoli Federico II, Napoli, Italia-
crisitem.author.deptDip. Sc. della Terra, Università di Napoli-
crisitem.author.deptDipartimento di Scienze della Terra e Università degli Studi “Federico II” di Napoli. Largo S. Marcellino 10, 80138 Napoli, Italy-
crisitem.author.deptDip. Sc. della Terra, Università di Napoli-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.orcid0000-0002-5880-7128-
crisitem.author.orcid0000-0002-5506-8753-
crisitem.author.orcid0000-0001-7133-0136-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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