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

tags: AZARBAIJAN SHARGHI