TECTONOPHYSICS, cilt.467, ss.1-21, 2009 (SCI-Expanded)
Understanding further the nature and evolution at lithospheric scale of the Sea of Marmara on the North Anatolian Fault needs constraints on the deep crustal and Mono spatial variation. This has been probed here with offshore-onshore and OBS, Ocean Bottom Seismometer refraction seismics, in addition to coincident MCS, marine multichannel reflection seismic profiles over the whole North Marmara Trough.