Anticline axes displacement between Fatha and Jeribe formation of structures In the south Hemreen area (Central Iraq ) from seismic evidence

The present study is concerned with interpretation of the available seismic data in the South Hemreen area ( Central Iraq ) , the aim of this study is to measure the amount of apparent anticline axes displacement between Fatha Formation (surface) and Jeribe Formation (sub surface), The maximum of the value is noted at the crest of the anticline , so 1250m , 1350m , and 2800m at crest Injana , Khashem Al-Ahmar and Munsuria anticlines respectively. While the horizontal stress ( NE-SW) was lead to folded and faulted the sedimentary cover and displace the Fatha Formation horizontally , where its salty rocks played an important role in this displacement.