“…While the eastern and northern regions of Iraq, which lie near the convergence borders of the Arabian and Eurasian plates, are subject to significant seismic activity, other regions of the country, which are farther from the plate boundary, are only subject to weak seismic activity [37]. The seismicity of Iraq has been studied by many researchers (for example, [38], [39], [35], [40], [41], [42], [43], [44]; [45], [46], [47], [48], Iraq is divided tectonically into three regions: the Bitlis-Zagros Fold and Thrust Belt, the Mesopotamia Foredeep, and the Inner (stable) Arabian platform (Figure 1) [52]. The Mesopotamia Foredeep is divided into the Al-Jazira Plain and the Mesopotamia Plain.…”