Active Tectonic Evidences in North Tabriz Fault Along
| Category | Tectonic & Seismotectonic |
|---|---|
| Group | GSI.IR |
| Location | 21th symposium on geosciences |
| Holding Date | 24 May 2008 |
Abstract:
Tabriz fault is one of the main geological structures in the northwest of Iran. Geomorphological evidences along this fault such as offset streams, pressure ridges and shutter ridges show that Tabriz fault is a dextral strike- slip fault and has young activities.
General:
Tabriz fault is one of the main geological structures in the northwest of Iran. Geomorphological evidences along this fault such as offset streams, pressure ridges and shutter ridges show that Tabriz fault is a dextral strike-slip fault and has young activities