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 |