We applied a 3-D seismic tomography inversion algorithm to arrival-time data obtained,
during 18 years from 1985 to 2002, from local seismic networks and aftershock studies in the …

Westward migration of large earthquakes along the North Anatolian Fault Zone seems to
have been suspended after the 1967 Mudurnu Valley earthquake, which may imply the …

Anisotropy of magnetic susceptibility (AMS) has been used to infer finite strain fabrics in
plastically deformed rocks, but there are few studies of magnetic properties in fractured fault …

Pseudotachylyte is a glassy fault rock providing certain evidence of ancient seismic fault
movement. I examine the Nojima pseudotachylyte found along the Nojima fault, which …

Observations of the geomagnetic total intensity have been carried out from time to time in a
possible seismic gap region in the western part of the North Anatolian Fault Zone (NAFZ), in …

In order to investigate changes in the geomagnetic field associated with seismic activity in
the western part of the North Anatolian Fault Zone (NAFZ), seven continuous measurement …

The North Anatolian Fault Zone (NAFZ) is a 1500 km long transform fault, and many right-
lateral strike-slip faults exist in the zone. Its overall activity has been considered as direct …

The second is the occurrence of two types of lineations found in the back-arc spreading
regions described as,(1) lineation& running parallel with the arc trend on a rifting or …

Observations of the geomagnetic total intensity, electric self-potential and surface resistivity
were carried out at the Atotsugawa fault, a 60 km long active fault of strike-slip type located …

The Wenner lateral resistivity and magnetic dyke profiles carried out along the southern
branch of the North Anatolian Fault System. The use of magnetic dyke method indicates that …