Geochemical evolution of upper tertiary basalts from Southern Lebanon - by Lara Moussa Kallas
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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.
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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
Bibliography : leaves 166-176
Bibliography : leaves 166-176