Neotectonic map of Syria and some aspects of Late Cenozoic evolution of the northwestern boundary zone of the Arabian plate

• Published in: Journal of geodynamics 2005-09, Vol.40 (2), p.235-256
• Main Authors: Rukieh, M., Trifonov, V.G., Dodonov, A.E., Minini, H., Ammar, O., Ivanova, T.P., Zaza, T., Yusef, A., Al-Shara, M., Jobaili, Y.
• Format: Article
• Language: English
• Subjects: Active faults; Neotectonic structure and phases of deformation in Syria
• ISSN: 0264-3707
• DOI: 10.1016/j.jog.2005.07.016

The neotectonic map of Syria, 1:500,000, was compiled by the authors in 2003–2004. The map shows tectonic features formed or continued to develop during the Neogene and Quaternary in Syria and adjacent territories, including the Mediterranean realm. The neotectonic structure of the region was formed as a result of three phases of deformation. During the Early Miocene first phase, the Arabian plate moved along the Dead Sea–Jordan segments of the Levant (Dead Sea) transform fault zone, Roum fault and its continuation in the continental slope of the Mediterranean. The chain of the coastal anticlines in the “Arabian” side of the transform zone and the Lattaqie oblique (sinistral-thrust) boundary fault zone in the north were formed under the NNW-trending compression. The Lattaqie zone continued by the Cyprus arc in the west and by the Taurus (Bitlis) thrust in the east and further by the Main Thrust of the Zagros. After “quiet” (for Syria) epoch of the Middle Miocene when the Arabian plate moved to the NE, during the Late Miocene second phase of deformation, the Arabian plate moved again to the NNW along the same transform boundary. But a part of the Late Miocene plate motion (up to 20 km) resulted by shortening in the Anti-Leban–Palmyride fold-thrust belt that separated the Aleppo block from the main part of the Arabian plate. During the Pliocene–Quaternary third phase of deformation, the recent structural pattern of the Levant zone was formed in Lebanon and the northwestern Syria. At the same time, the Serghaya and smaller sinistral faults branched out the Levant zone and the system of the W–E-trending convex to the south dextral faults ruptured the Palmyrides and the stable part of the Arabian plate. The total Pliocene–Quaternary sinistral offset on the young Levant zone segments and the associated faults has reached 35–40 km, like on the Dead Sea–Jordan segments of the Levant fault zone. The faults, demonstrating the Pliocene–Quaternary activity are still active now and represent the main seismic zones in Syria. Offsets on them are mostly a cumulative effect of strong earthquakes.