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Structural analysis of latitudinal faults in the Mount Lebanon north of Beirut their kinematics and their role in the tectonic evolution of Lebanon - by Martin Atallah Gedeon

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dc.contributor.author Gedeon, Martin Atallah
dc.date.accessioned 2012-06-13T06:45:52Z
dc.date.available 2012-06-13T06:45:52Z
dc.date.issued 1999
dc.identifier.uri http://hdl.handle.net/10938/5691
dc.description Thesis (M.S.)--American University of Beirut. Department of Geology, 1999;"Advisor: Dr. Sara Spencer, Assistant Professor, Geology--Member of Committee: Dr. Kamal Khair, Lecturer , Geology--Member of Committee: Dr. Mohamed Harajli, Professor, Civil Engine
dc.description Bibliography : 218-226
dc.description.abstract Lebanon is situated on a major plate boundary between the Arabian and the Levantine plates. This is known to be a seismically active region accommodating part of the Arabian plate rotation through strike-slip faulting along the Dead Sea Transform Fault. M
dc.format.extent xix, 226 leaves : ill. (some col.), tables
dc.language.iso eng
dc.relation.ispartof Theses, Dissertations, and Projects
dc.subject.classification T:003967 AUBNO
dc.subject.lcsh Faults (Geology) -- Lebanon -- Mount Lebanon
dc.subject.lcsh Plate tectonics -- Lebanon
dc.subject.lcsh Kinematics
dc.title Structural analysis of latitudinal faults in the Mount Lebanon north of Beirut their kinematics and their role in the tectonic evolution of Lebanon - by Martin Atallah Gedeon
dc.type Thesis
dc.contributor.department American University of Beirut. Faculty of Arts and Sciences. Department of Geology


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