Abstract
A detailed interpretation of seismic data in the Euphrates Graben Area (intra the northern margin of Arabian plate) has contributed to describe the tectono-depositional evolution. The stratigraphic sequences from the Paleozoic to recent time within the Euphrates Graben are composed of a number of discrete depositional cycles separated by nondeposition and/or erosional surfaces. This graben could be divided into several categories of structural units based on the degree of deformation and structural geometry. Intensive extensional tectonic activities have caused to create the NW–SE trending Euphrates Rift System in the Late Cretaceous and associated with volcanic intrusion which was distinguished by chaotic reflections on seismic profiles. Furthermore, it led to deposit of continental Derro Rocks. During this period, the Judea and Rutbah Formations exposed to erosion processes left behind unconformity surface at base of Upper Cretaceous is called BKU Unconformity. The Euphrates Graben Area had also exposed uplift events in Palaeozoic time in which volcanic intrusions played an essential role in uplift of some of the Euphrates Area parts as indicated restoration model.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
