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in the fault bend area
The North Anatolian Fault trace and related geological and geomorphological offsets defining a 80 to 100 km total slip. In the east
the suture zone
defined an offset of about 85 km.
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From Hubert et al. JGR 107 (2002) doi: 10.1029/2001JB000393
in the west
in the Erbaa pull-apart area
in the east
Offsets
:
Collaboration
Team
Seismicity Switching
Extrusion Tectonic
Introduction
North Anatolian Fault
Seismic Cycle
Field Work
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