Holocene Sedimentary and Gravitative Processes in Highstand Prodelta Deposits on the Cuma outer shelf (Eastern Tyrrhenian sea, Italy): An Integrated Approach (Articolo in rivista)

Type
Label
  • Holocene Sedimentary and Gravitative Processes in Highstand Prodelta Deposits on the Cuma outer shelf (Eastern Tyrrhenian sea, Italy): An Integrated Approach (Articolo in rivista) (literal)
Anno
  • 2011-01-01T00:00:00+01:00 (literal)
Alternative label
  • Emanuela Petruccione; Gemma Aiello; Giovanna Capretto; Maria Rosaria Senatore; Ennio Marsella; Marina Iorio (2011)
    Holocene Sedimentary and Gravitative Processes in Highstand Prodelta Deposits on the Cuma outer shelf (Eastern Tyrrhenian sea, Italy): An Integrated Approach
    in DTA; CNR-Dipartimento terra e ambiente, Roma (Italia)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Emanuela Petruccione; Gemma Aiello; Giovanna Capretto; Maria Rosaria Senatore; Ennio Marsella; Marina Iorio (literal)
Pagina inizio
  • 771 (literal)
Pagina fine
  • 784 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
  • Collana: \"Marine Research at CNR\", Volume Mare - CNR Dipartimento Terra e Ambiente, DTA ISSN Collana: 2239-5172 Ultimo autore (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • DTA/06-2011 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#descrizioneSinteticaDelProdotto
  • Articolo non ISI con referee (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Istituto per l'Ambiente Marino Costiero, CNR, Napoli, Italy Dipartimento di Studi Geologici ed Ambientali, Università del Sannio, Benevento, Italy (literal)
Titolo
  • Holocene Sedimentary and Gravitative Processes in Highstand Prodelta Deposits on the Cuma outer shelf (Eastern Tyrrhenian sea, Italy): An Integrated Approach (literal)
Abstract
  • High resolution seismic profiles interpretation and sedimentological and petrophysical correlation of piston cores has been carried out to define sedimentary and gravitative processes in a prodelta area of the Cuma offshore. This unit is constituted in the upper part by mud deposits, which are affected by a downward-displacement cropping out at the sea bottom, related to creep-type processes. The integrated approach (sedimentologic, petrophysic and seismostratigraphic analysis) allowed to establish that the sedimentological body interested by the deformation preserved an internal geometry testifying a low sliding of the sedimentary body without reworking. Moreover the emplacement of the upper unit, characterized by mud deposits, is interpreted as controlled by high sediment supply, high water contents and shallow gas pockets which could represent a principal triggering factor of the submarine instabilities. (literal)
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