Tectonics of Strike-Slip Restraining & Releasing Bends in Continental & Oceanic Settings (D. Cunningham & P. Mann, eds.)
Geological Society Special Publication (2007, v. 290, p. 285 - 303)

Strain partitioning of active transpression within the Lebanese Restraining Bend of the Dead Sea fault (Lebanon and SW Syria)

Francisco Gomez1, Tony Nemer1, Charles Tabet2, Mohamad Khawlie3, Mustapha Meghraoui4, Muawia Barazangi5

1Department of Geological Sciences, University of Missouri, Columbia, Missouri  65211, USA (e-mail: fgomez@missouri.edu)
2Lebanese National Council for Scientific Research, Beirut, Lebanon
3Lebanese National Center for Remote Sensing, Beirut, Lebanon
4EOST, Institut de Physique du Globe, UMR 7516, Strasbourg, France
5Institute for the Study of the Continents, Snee Hall, Cornell University, Ithaca, New York  14853, USA

Abstract
Recent neotectonic, palaeoseismic, and GPS results along the central Dead Sea fault system elucidate the spatial distribution of crustal deformation within a large (~180 km long) restraining bend along this major continental transform.  Within the “Lebanese” restraining bend, the Dead Sea fault system splays into several key branches, and we suggest herein that active deformation is partitioned between NNE-SSW strike-slip faults and WNW-ESE crustal shortening.  When plate motion is decomposed into strike-slip parallel to the two prominent NNE-SSW strike-slip faults (the Yammouneh and Serghaya faults) and orthogonal motion, their slip rates are sufficient to account for all expected strike-slip motion.  Shortening of the Mount Lebanon range is inferred from the geometry and kinematics of the Roum fault, as well as preliminary quantification of coastal uplift.  The results do not account for all expected crustal shortening, suggesting that some contraction is likely accommodated in the Anti Lebanon range.  It also seems unlikely that the present kinematic configuration characterizes the entire Cenozoic history of the restraining bend.  Present-day strain partitioning contrasts with published observations on finite deformation in Lebanon demonstrating distributed shear and vertical-axis block rotations.  Furthermore, the present-day proportions of strike-slip displacement and crustal shortening are inconsistent with the total strike-slip offset and the lack of a significantly thickened crust.  This suggests that the present rate of crustal shortening has not persisted for the longer life of the transform.  Hence, we suggest that the Lebanese restraining bend evolved in a polyphase manner:  An earlier episode of wrench-faulting and block rotation, followed by the later period of strain partitioning.

Return to publication list

Return to main page