Ultra nagy felbontású reflexiós szeizmikus képalkotás haszna és szépségei: Késő-negyedidőszaki tengeri vulkanoklasztos felépítmények a Nápolyi-Öbölben

Translated title of the contribution: The use and beauty of ultra-high-resolution seismic reflection imaging in late quaternary marine volcaniclastic settings, bay of Naples, Italy

Marco Sacchi, Mauro Caccavale, Marta Corradino, Giuseppe Esposito, Luigi Ferranti, Zoltán Hámori, Ferenc Horváth, Donatella Insinga, Camilla Marino, Fabio Matano, Flavia Molisso, Jacopo Natale, Salvatore Passaro, Fabrizio Pepe, Tamás Tóth

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

Very high-resolution, single channel (IKB-Seistec™) reflection seizmic profiles acquired in the Bay of Naples, com-plemented with geological and geophysical data from the literature, provide unprecedented, superb seismic imaging of the latest Pleistocene–Holocene stratigraphic architecture of the submerged sectors Campi Flegrei and Somma-Vesuvius volcanic districts. Seismic profiles were calibrated by gravity core data and document a range of depositional systems, volcanic structures and hydrothermal features that evolved after the onset of the Last Glacial Maximum (~ 18 ka BP) over the continental shelf on the Campania coastal zone. Seistec profiles from the Pozzuoli Bay yield high-resolution images of the shallow structure of the collapse caldera-ring fault — resurgent dome system associated with the eruption of the Neapolitan Yellow Tuff (NYT) (ca 15 ka) and support a working hypothesis to assess the timing and the styles of deformation of the NYT resurgent structure throughout the latest Quaternary. Seismic images also revealed the nature of the fragile deformation of strata along the NYT ring fault system and the occurrence of hydrothermal fluids and volcanic/subvolcanic intrusions ascending along the ring fault zone. Seismic data acquired over the continental shelf off the Somma-Vesuvius stratovolcano, display evidence of gravitational instability of wavy bedforms representing the submarine prosecution of pyroclastic flows originated from the Vesuvius during the eruption that destroyed the Roman city of Herculaneum in 79 CE. At the Banco della Montagna, a hummocky seafloor knoll located between the Somma-Vesuvius and the Pozzuoli Bay, seismic profiles and gravity core data revealed the occurrence of a field of volcaniclastic diapirs formed by the dragging and rising up of unconsolidated pumice, as a consequence of fluid overpressure at depth associated with active degassing and fluid venting at the seafloor.

Translated title of the contributionThe use and beauty of ultra-high-resolution seismic reflection imaging in late quaternary marine volcaniclastic settings, bay of Naples, Italy
Original languageHungarian
Pages (from-to)371-394
Number of pages24
JournalFoldtani Kozlony
Volume149
Issue number3
DOIs
Publication statusPublished - Jan 1 2019

ASJC Scopus subject areas

  • Geology
  • Geochemistry and Petrology
  • Stratigraphy
  • Palaeontology

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    Sacchi, M., Caccavale, M., Corradino, M., Esposito, G., Ferranti, L., Hámori, Z., Horváth, F., Insinga, D., Marino, C., Matano, F., Molisso, F., Natale, J., Passaro, S., Pepe, F., & Tóth, T. (2019). Ultra nagy felbontású reflexiós szeizmikus képalkotás haszna és szépségei: Késő-negyedidőszaki tengeri vulkanoklasztos felépítmények a Nápolyi-Öbölben. Foldtani Kozlony, 149(3), 371-394. https://doi.org/10.23928/foldt.kozl.2019.149.4.371