Late Cenozoic uplift along the northern Dead Sea transform in Lebanon and Syria |
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| Institution: | 1. Berger Geosciences, 13100 Northwest Freeway, Houston, TX 77040, USA;2. Department of Earth and Atmospheric Sciences, University of Houston, TX 77004, USA;3. Department of Geology, University of Cincinnati, Cincinnati, OH 45221, USA;4. Center of Excellence in Mineralogy, University of Baluchistan, Pakistan;5. Department of Physics, Purdue University, West Lafayette, IN 47907, USA;1. First Crust Deformation Monitoring and Application Center, CEA, Tianjin, China;2. CEA Key Laboratory of Earthquake Prediction (Institute of Earthquake Science, China Earthquake Administration), Beijing, China;1. Centre de Recherche Pétrographique et Géochimique, Université de Lorraine - CNRS, UMR 7358, 15 rue Notre Dame des Pauvres, B.P. 20, 54501 Vand?uvre lès Nancy, France;2. University of Montpellier, Géosciences Montpellier, UMR 5243, Place E. Bataillon, case 060, 34095 Montpellier Cedex 5, France;3. California Institute of Technology, Division of Geology and Planetary Sciences, 1200 E California Blvd, Pasadena, CA 91125, United States;4. University of California, Department of Earth, Planetary and Space Sciences, Los Angeles, CA 90095-1567, United States;5. Nanjing University, Department of Earth and Sciences, Nanjing, China;6. Department of Geography, University of Sheffield, Sheffield S10 2TN, UK |
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| Abstract: | Evidence of long-term, late Cenozoic uplift, as well as strike-slip faulting, is revealed by topographic and geological features along the northern 500 km of the Dead Sea fault system (DSFS)—the transform boundary between the Arabian and African plates in the eastern Mediterranean region. Macro-geomorphic features are studied using a new, high-resolution (20 m pixel) digital elevation model (DEM) produced by radar interferometry (InSAR). This DEM provides a spatially continuous view of topography at an unprecedented resolution along this continental transform from 32.5° to 38° N. This section of the left-lateral transform can be subdivided into a 200 km long Lebanese restraining bend (mostly in Lebanon), and the section to the north (northwest Syria). Spatial variations in Cenozoic bedrock uplift are inferred through mapping of topographic residuals from the DEM. Additionally, high altitude, low-relief surfaces are mapped and classified in the Mount Lebanon and Anti Lebanon ranges that also provide references for assessing net uplift. These results demonstrate an asymmetric distribution of post-Miocene uplift between the Mt. Lebanon and Anti Lebanon ranges. Antecedent drainages also imply that a major episode of uplift in the Palmyride fold belt post-dates the uplift of the Anti Lebanon region. North of the restraining bend, the Late Miocene surface is preserved beneath spatially extensive lava flows. Hilltop remnants of this paleosurface demonstrate Pliocene-Quaternary uplift and tilting of the Syrian Coastal Range, adjacent to the DSFS north of the restraining bend. This late Cenozoic uplift is contemporaneous with strike-slip along the DSFS. Geometrical relationships between folds and strike-slip features suggest that regional strain partitioning may accommodate a convergent component of motion between the Arabian and African plates. This interpretation is consistent with regional plate tectonic models that predict 10–25° of obliquity between the relative plate motion and the strike of the DSFS north of the restraining bend. We suggest that this convergent component of plate motion is responsible for uplift along and adjacent to the DSFS in the Syrian Coastal Range, as well as within the Lebanese restraining bend. |
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