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 |