Wathiq GH. ABDULNABY - Seismological Unit of University of Basrah (SCUB) Department of Geology, College of Sciences, University of Basrah, Basrah, Iraq
Maher M. MAHDI - Seismological Unit of University of Basrah (SCUB)Department of Geology, College of Sciences, University of Basrah, Basrah, Iraq
Rafed AL-MOHMED - Seismological Unit of University of Basrah (SCUB)Department of Geology, College of Sciences, University of Basrah, Basrah, Iraq

The Badra-Amarah fault is located in the northeastern side of the Mesopotamian Zone at the Iraq-Iran border. This fault is the most seismically active fault in Iraq and it is located within the zone of the major damage. The goal of this study is to study the seismic history, focal mechanism solutions, and the recent stress analysis of the Badra-Amarah fault. The seismic history has been studied by using the source parameters of earthquakes from different catalogs, mainly from the IRSC catalog. The focal mechanism solutions were calculated from the CMT catalog, which were analyzed in this study to derive the principal stress directions and their regimes. According the seismic history of the study area, four seismic swarms occurred at the fault in August, 2008, June, 2009, August, 2009, and April, 2012 with magnitude of main shocks ranges from 4.4 to 5.7. The focal mechanism solutions show that the Badra -Amarah fault has a reverse movement with little strike-slip displacement. The dip of the fault is 60° with dip direction equals 226°. From the stress inversion of moment tensors, the principal stress axes are: σ1 is 14°/217°, σ2 is 10°/309°, and σ3 is 72°/074°. The length of fault is about 200 km and its depth may reach the basement rocks which are about 10 km.

Seismotectonics of Iraq, Focal Mechanism Solutions, Stress Analyses, Arabian Plate, Badra-Amara Fault.