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Aiello, G., Angelino, A., Budillon, F., Cappelletti, P., Conforti, A., Cristofalo, G., De Lauro, M., Ferraro, L., Insinga, D., Marsella, E., Molisso, F., Montella, R., Morra, V., Musella, S., Nicotra, G., Pelosi, N., Pinto, C., Rapisarda, S., Ricci, G., Russo, L., Sacchi, M., Santoro, G., Sarnacchiaro, G., Sclafani, P., Tonielli, R. and Toscano, F. (1999) Campionature del fondo mare e prospezioni geofisiche nell’area dei Golfi di Napoli e Salerno. Istituto di Ricerca Geomare Sud, Rapporto Tecnico No. 9, Crociera Oceanografica GMS98-01, Napoli, Dicembre 1999.

has been cited by the following article:

• TITLE: Magnetic Theory and Applications in the Naples Bay (Southern Tyrrhenian Sea, Italy): Magnetic Anomaly Fields and Relationships with Morpho-Structural Lineaments

  AUTHORS: Gemma Aiello, Ennio Marsella

  KEYWORDS: Magnetic Anomaly, Naples Bay, Southern Tyrrhenian Sea

  JOURNAL NAME: World Journal of Condensed Matter Physics, Vol.6 No.3, August 9, 2016

  ABSTRACT: Magnetic theory and application to a complex volcanic area located in Southern Italy are here discussed showing the example of the Gulf of Naples, located at Southern Italy Tyrrhenian margin. A magnetic anomaly map of the Gulf of Naples has been constructed aimed at highlighting new knowledge on geophysics and volcanology of this area of the Eastern Tyrrhenian margin, characterized by a complex geophysical setting, strongly depending on sea bottom topography. The theoretical aspects of marine magnetometry and multibeam bathymetry have been discussed. Magnetic data processing included the correction of the data for the diurnal variation, the correction of the data for the offset and the leveling of the data as a function of the correction at the cross-points of the navigation lines. Multibeam and single-beam bathymetric data processing has been considered. Magnetic anomaly fields in the Naples Bay have been discussed through a detailed geological interpretation and correlated with main morpho-structural features recognized through morpho- bathymetric interpretation. Details of magnetic anomalies have been selected, represented and correlated with significant seismic profiles, recorded on the same navigation lines of magnetometry. They include the continental shelf offshore the Somma-Vesuvius volcanic complex, the outer shelf of the Gulf of Pozzuoli offshore the Phlegrean Fields volcanic complex, the relict volcanic banks of Pentapalummo, Nisida and Miseno, the Gaia volcanic bank on the Naples slope, the western slope of the Dohrn canyon, the Magnaghi canyon’s head and the magnetic anomalies among the Ischia and Procida islands.