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In this study we integrate high-resolution swath bathymetry, single channel reflection seismic data and gravity core data, to provide new insights into the shallow structure and latest Quaternary to Holocene evolution of the submerged sector of the Neapolitan Yellow Tuff (NYT) caldera (Campi Flegrei) in the Pozzuoli Bay.
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Figure 4: Interpreted W-NE striking multi-channel reflection seismic profile across the SW strait.
Focuses on synthetic seismograms, ocean bottom refraction seismology, and multi-channel reflection seismology as applied to studies of the ocean sediments, crust, and lithosphere.
Single-channel reflection seismic profiles provided information on the sediment wave internal structure and the Quaternary stratigraphic architecture of the GoR outer shelf and slope.
(d) Seismic profile perpendicular to the strait axis, showing caldera-fill stratigraphic units 1 and 2 of ref. 10. Figure 3: Interpreted multi-channel reflection seismic profile along the axis of the NW strait.
To investigate the history of the Aare Glacier and its overdeepened valley, a high-resolution multibeam bathymetric dataset and a 2D multi-channel reflection seismic dataset were acquired on perialpine Lake Thun Switzerlandd).
Hypocenter locations were projected on time-migrated section along four multi-channel reflection survey lines (Nakamura et al., 2011; 2013).
Although they form a unique geomorphic province, identifying seismogenic faults and interpreting the tectonic condition should be based on fault morphology in the deep interior of the basin through the use of multi-channel reflection seismic data.
Compared with the time-migrated sections of multi-channel reflection surveys (Nakamura et al., 2011; 2013), the shallow earthquakes landward of the trench axis mainly occurred in the oceanic crust (Figure 3).
We also used 2D multi-channel reflection data acquired during cruise ODKM-03 by the R/V Polar Princess in 2003, which employed a tuned airgun array with a total volume of approximately 70 L (4,240 in3) fired at 50-m intervals and a 6-km-long streamer with 480 channels.
In the Bay of Naples the sequence stratigraphy interpretation of more than 4000 km of single-channel and multi-channel seismic reflection profiles made it possible to reconstruct the three-dimensional architecture of the ignimbrite units.
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