The Regional Geological Structure of the Naples Bay Inferred by New Multichannel Seismic Reflection Profiles (Articolo in rivista)

Type
Label
  • The Regional Geological Structure of the Naples Bay Inferred by New Multichannel Seismic Reflection Profiles (Articolo in rivista) (literal)
Anno
  • 2011-01-01T00:00:00+01:00 (literal)
Alternative label
  • Gemma Aiello; Anna Giuseppa Cicchella; Vincenzo Di Fiore; Ennio Marsella (2011)
    The Regional Geological Structure of the Naples Bay Inferred by New Multichannel Seismic Reflection Profiles
    in DTA
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Gemma Aiello; Anna Giuseppa Cicchella; Vincenzo Di Fiore; Ennio Marsella (literal)
Pagina inizio
  • 573 (literal)
Pagina fine
  • 583 (literal)
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  • Articolo su rivista nazionale con referee (literal)
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  • DTA6/2011 (literal)
Rivista
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  • Articolo non ISI con referee (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • CNR-IAMC Sede di Napoli (literal)
Titolo
  • The Regional Geological Structure of the Naples Bay Inferred by New Multichannel Seismic Reflection Profiles (literal)
Abstract
  • The deep regional geological structure of the Naples Bay is controlled by two NE-SW and NNE-SSW (Anti-Apenninic) normal faults, the Dohrn canyon fault and the Capri-Sorrento fault. Strong downthrows of Meso-Cenozoic sedimentary sequences, representing the acoustic basement, have been observed in correspondence to both the faults. Main regional morpho-structures are: the Banco di Fuori, a morpho-structural high of the Meso-Cenozoic carbonatic acoustic basement, bounding southwards the Naples Bay, whose flanks and top are draped by the Pleistocene deposits of the Late Quaternary sequence; the Dohrn canyon, separating the eastern side of the Bay, where sedimentary seismic sequences crop out, from the western one, where volcanic seismic units prevail; the Magnaghi canyon, draining the volcanic and volcano-clastic input of the Ischia and Procida islands during the Late Quaternary and eroding the sediments of the Mg volcanic unit, characterized by chaotic reflectors; the Capri Basin, a deep basin localised in the Tyrrhenian bathyal plain south of the Naples Bay in the southern sector of the Dohrn Canyon, infilled by Pleistocenic-Holocenic sediments overlying the carbonatic basement; the Salerno Valley, a half-graben filled by three seismic units corresponding to Quaternary marine and continental deposits, laterally grading to chaotic sequences related to the \"Flysch del Cilento\" Auct.; the Volturno Basin, infilled by four marine to deltaic seismic sequences, frequently alternating with volcanoclastic levels, overlying deep seismic units, correlated with Miocene flysch deposits (sands and shales) and Meso-Cenozoic carbonates. (literal)
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