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Geochemical evolution of upper tertiary basalts from Southern Lebanon - by Lara Moussa Kallas

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dc.contributor.author Kallas, Lara Moussa
dc.date.accessioned 2012-06-13T07:04:55Z
dc.date.available 2012-06-13T07:04:55Z
dc.date.issued 2001
dc.identifier.uri http://hdl.handle.net/10938/6125
dc.description Thesis (M.S.)--American University of Beirut. Department of Geology, 2001;"Advisor: Dr. Abdel-Fattah M. Abdel-Rahman, Associate Professor, Geology--Member of Committee: Dr. Amir Mokhtary-Fard,Assistant Professor, Geology--Member of Committee: Dr. Ulrich K
dc.description Bibliography : leaves 166-176
dc.description.abstract The Upper Tertiary basaltic flows are located in the western Bekaa valley, and occur within Neogene limestone strata. The rocks occur in a number of flows reaching two meters in thickness. The flows contain both highly vesicular to massive basaltic rocks.
dc.format.extent x, 176 leaves : ill. (some col.), tables
dc.language.iso eng
dc.relation.ispartof Theses, Dissertations, and Projects
dc.subject.classification T:004151 AUBNO
dc.subject.lcsh Basalt -- Lebanon -- South
dc.subject.lcsh Geology, Stratigraphic -- Tertiary
dc.subject.lcsh Geochemistry -- Lebanon
dc.title Geochemical evolution of upper tertiary basalts from Southern Lebanon - by Lara Moussa Kallas
dc.type Thesis
dc.contributor.department American University of Beirut. Faculty of Arts and Sciences. Department of Geology


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