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Investigating the Geological Fault Framework Offshore Lebanon: Insight into the Earthquake Geology of the Region

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dc.contributor.advisor Nemer, Tony
dc.contributor.author Faysal, Reenal
dc.date.accessioned 2022-09-14T04:55:40Z
dc.date.available 2022-09-14T04:55:40Z
dc.date.issued 9/14/2022
dc.date.submitted 9/13/2022
dc.identifier.uri http://hdl.handle.net/10938/23580
dc.description.abstract The tectonic setting of Lebanon in the eastern Mediterranean region is a restraining bend along the Dead Sea Transform Fault, which is the plate boundary between Arabia and Africa. Within the Lebanese Restraining Bend, the plate boundary splays into several fault branches that are mapped onshore Lebanon and known to have contributed to the evolution of the Lebanese structural framework. However, little is known about the geological structures offshore Lebanon, and how those structures could relate to the onshore tectonics. Such information is very useful in understanding the tectonic framework of the region from two perspectives: (1) earthquake geology and (2) petroleum geology. The objective of this thesis is to investigate and study, through 3D seismic interpretation, the tectonic framework offshore Lebanon. This provides a wealth of needed insight into the earthquake geology of the region. In addition, mapping the faults offshore Lebanon and understanding their tectonic behavior can provide valuable comprehension of the elements of the hydrocarbon systems in the Lebanese part of the Levant basin. A bathymetric map of the Lebanese offshore area is generated and used to delineate the faults’ surface features. The major and minor faults are interpreted and used to identify and understand the behavior of potential tsunami-generating structures. A previously interpreted thrust fault system offshore Lebanon referred to as ‘Mount Lebanon thrust’ was suggested to be responsible for the A.D. 551 earthquake, which was one of the most destructive in the history of the Levant. After careful investigation of the offshore area using 3D seismic data, we believe that this system is more a hypothesis than a reality. In addition, we propose that the Latakia ridge is a prominent structure that can trigger such tsunamigenic earthquakes. This thesis provides some insight into the earthquake and tsunami generation potential in the eastern Mediterranean area, together with additional input into future investigations of the hydrocarbon potential offshore Lebanon.
dc.language.iso en
dc.subject Faults
dc.subject Lebanon
dc.subject Offshore Lebanon
dc.subject 3D seismic
dc.subject seismic interpretation
dc.subject structures
dc.subject Levant basin
dc.subject Dead Sea Transform Fault
dc.subject earthquake geology
dc.subject tsunami
dc.subject A.D. 551 earthquake
dc.subject Lebanese Restraining Bend
dc.subject tectonics
dc.subject petroleum geology
dc.subject tsunamigenic earthquakes
dc.subject geologic framework
dc.subject geology
dc.title Investigating the Geological Fault Framework Offshore Lebanon: Insight into the Earthquake Geology of the Region
dc.type Thesis
dc.contributor.department Department of Geology
dc.contributor.faculty Faculty of Arts and Sciences
dc.contributor.institution American University of Beirut
dc.contributor.commembers Abdel-Rahman, Abdel-Fattah
dc.contributor.commembers Salah, Mohamed
dc.contributor.degree MS
dc.contributor.AUBidnumber 201707012


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