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dc.contributor.authorAmato, Vincenzoes_ES
dc.contributor.authorAucelli, P.P.C.es_ES
dc.contributor.authorCesarano, M.es_ES
dc.contributor.authorFilocamo, F.es_ES
dc.contributor.authorLeone, N.es_ES
dc.contributor.authorPetrosino, P.es_ES
dc.contributor.authorRosskopf, C.M.es_ES
dc.contributor.authorValente, E.es_ES
dc.contributor.authorCasciello, Emilioes_ES
dc.contributor.authorGiralt, Santiagoes_ES
dc.contributor.authorJicha, B. R.es_ES
dc.date.accessioned2018-09-20T09:33:02Z-
dc.date.available2018-09-20T09:33:02Z-
dc.date.issued2018-
dc.identifier.citationEarth Surface Processes and Landforms, 43(11): 2463-2480 (2018)es_ES
dc.identifier.issn0197-9337-
dc.identifier.urihttp://hdl.handle.net/10261/169923-
dc.description.abstractThe present study focuses on the morphotectonic evolution of the axial portion of the Southern Apennine chain between the lower Calore River valley and the northern Camposauro mountain front (Campania Region). A multidisciplinary approach was used, including geomorphological, field-geology, stratigraphical, morphotectonic, structural, Ar-40/Ar-39 and tephrostratigraphical data. Results indicate that, from the Lower Pleistocene onwards, this sector of the chain was affected by extensional tectonics responsible for the onset of the sedimentation of Quaternary fluvial, alluvial fan and slope deposits. Fault systems are mainly composed of NW-SE, NE-SW and W-E trending strike-slip and normal faults, associated to NW-SE and NE-SW oriented extensions. Fault scarps, stratigraphical and structural data and morphotectonic indicators suggest that these faults affected the wide piedmont area of the northern Camposauro mountain front in the Lower Pleistocene-Upper Pleistocene time span. Faults affected both the oldest Quaternary slope deposits (Laiano Synthem, Lower Pleistocene) and the overlying alluvial fan system deposits constrained between the late Middle Pleistocene and the Holocene. The latter are geomorphologically and chrono-stratigraphically grouped into four generations, I generation: late Middle Pleistocene-early Upper Pleistocene, with tephra layers Ar-40/Ar-39 dated to 158 +/- 6 and 113 +/- 7 ka; II generation: Upper Pleistocene, with tephra layers correlated with the Campanian Ignimbrite (39ka) and with the slightly older Campi Flegrei activity (Ar-40/Ar-39 age 48 +/- 7 ka); III generation: late Upper Pleistocene-Lower Holocene, with tephra layers correlated with the Neapolitan Yellow Tuff (15ka); IV generation: Holocene in age. The evolution of the first three generations was controlled by Middle Pleistocene extensional tectonics, while Holocene fans do not show evidence of tectonic activity. Nevertheless, considering the moderate to high magnitude historical seismicity of the study area, we cannot rule out that some of the recognized faults may still be active. Copyright (c) 2018 John Wiley & Sons, Ltd.es_ES
dc.language.isoenges_ES
dc.publisherJohn Wiley & Sonses_ES
dc.rightsclosedAccesses_ES
dc.subjectgeomorphologyes_ES
dc.subjectextensional tectonicses_ES
dc.subjectAlluvial fanses_ES
dc.subjecttephrostratigraphyes_ES
dc.subjectsouthern Italyes_ES
dc.titleGeomorphic response to late Quaternary tectonics in the axial portion of the Southern Apennines (Italy): A case study from the Calore River valleyes_ES
dc.typeartículoes_ES
dc.identifier.doi10.1002/esp.4390-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi-org.sire.ub.edu/10.1002/esp.4390es_ES
dc.identifier.e-issn1096-9837-
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.contributor.orcidCasciello, Emilio [0000-0002-6086-3487]es_ES
dc.contributor.orcidGiralt, Santiago [0000-0001-8570-7838]es_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairetypeartículo-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextnone-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextNo Fulltext-
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