dc.contributor.author |
Harb, Mahmoud Hasan |
dc.date.accessioned |
2012-06-13T06:47:51Z |
dc.date.available |
2012-06-13T06:47:51Z |
dc.date.issued |
2001 |
dc.identifier.uri |
http://hdl.handle.net/10938/6046 |
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 Kor |
dc.description |
Bibliography : leaves 157-165 |
dc.description.abstract |
Mafic rocks of Bae'r-Bassit complex (NW Syria) occur as a part of a well-defined ophiolitic sequence in the region. The mafic rocks are present mainly as massive poorly layered isotropic gabbros, sheeted dykes, and minor pillow lavas. The gabbroic rocks v |
dc.format.extent |
xiv, 165 leaves : ill. (some col.), tables |
dc.language.iso |
eng |
dc.relation.ispartof |
Theses, Dissertations, and Projects |
dc.subject.classification |
T:004136 AUBNO |
dc.subject.lcsh |
Petrology -- Syria |
dc.subject.lcsh |
Geochemistry -- Syria |
dc.subject.lcsh |
Ophiolites -- Syria |
dc.title |
Petrology and geochemistry of the Mafic Unit of the Baer-Bassit Ophiolithic Complex, Northwestern Syria - by Mahmoud Hasan Harb |
dc.type |
Thesis |
dc.contributor.department |
American University of Beirut. Faculty of Arts and Sciences. Department of Geology |