The Yenice-Gonen active fault (NW Turkey): Active tectonics and palaeoseismology


Kuercer A., Chatzipetros A., Tutkun S. Z. , Pavlides S., Ates O. , Valkaniotis S.

TECTONOPHYSICS, cilt.453, ss.263-275, 2008 (SCI İndekslerine Giren Dergi) identifier identifier

  • Cilt numarası: 453
  • Basım Tarihi: 2008
  • Doi Numarası: 10.1016/j.tecto.2007.07.010
  • Dergi Adı: TECTONOPHYSICS
  • Sayfa Sayıları: ss.263-275

Özet

The Yenice-Gonen Fault (YGF) is one of the most important active tectonic structures in the Biga peninsula. On March 18,1953, a destructive earthquake (M-w=7.2) occurred on the YGF, which is considered to be a part of the southern branch of the North Anatolian Fault Zone (NAFZ). A 70 km-long dextral surface rupture formed during the Yenice-Gonen Earthquake (YGE).