Fluid flow, deformation rates and the submarine record of major earthquakes in the Sea of Marmara, along the North-Anatolian Fault system


Gasperini L., Polonia A., Çağatay M. N.

DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, cilt.153, ss.4-16, 2018 (SCI İndekslerine Giren Dergi) identifier identifier

  • Cilt numarası: 153
  • Basım Tarihi: 2018
  • Doi Numarası: 10.1016/j.dsr2.2018.03.004
  • Dergi Adı: DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
  • Sayfa Sayıları: ss.4-16

Özet

The submerged portions of the North-Anatolian Fault (NAF) in the Sea of Marmara and the NE-Aegean Sea are sites of large magnitude earthquakes, that leave diagnostic geological "signatures" in the sedimentary record in the form of mass-wasting deposits, turbidites, and fluid and gas escape features. This is due to the interplay of seismic-shaking, mass- and turbidity flows, sediment resuspension and fluids circulation in relatively small subbasins with a complex paleo-oceanography, steep slopes, high rates of deformation, and diffuse fault-controlled gas and fluid seeps. To unravel the complex interrelations of these phenomena during earthquake cycles, we carried out paleoseismological studies at several key locations.