Investigation on the tectonic significance of Izmir,Uzunada Fault Zones and other tectonic elements in the Gulf of Izmir,western Turkey,using high resolution seismic data |
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| Institution: | 1. Dipartimento di Scienze, Università Roma Tre, Roma, Italy;2. Géosciences Rennes, UMR 6118, Université de Rennes 1, Rennes, France;3. Institut für Geowissenschaften, Goethe-Universität, Frankfurt am Main, Germany;4. Institut für Mineralogie und Kristallchemie, Universität Stuttgart, Stuttgart, Germany;1. Dept of Geography, University of Liège, allée du 6 août 2, 4000 Liège, Belgium;2. ISTerre, CNRS UMR 5275, University of Savoie, F-73376 Le Bourget du Lac, France;3. LSCE, CNRS UMR 8212, avenue de la Terrasse, 91198, F-91191 Gif-sur-Yvette, France;4. Istituto Nazionale di Geofisica e Vulcanologia, Via E. Bassini, 15, 20133 Milano, Italy;5. EDYTEM, University of Savoie/CNRS, Le Bourget du Lac, France;6. Shell U.K. Limited, London, United Kingdom;7. Institute of Oceanography, Hellenic Center for Marine Research, GR-19013 Anavyssos, Greece;8. Institut de Radioprotection et de Sûreté Nucléaire (IRSN), Fontenay-aux-Roses, France;1. CSIR—National Geophysical Research Institute, Hyderabad 500007, India;2. Earth and Climate Science Program, Indian Institute of Science Education & Research—Pune, Homi Bhabha Road, Pune 411008, India;3. Indian Institute of Science Education & Research—Kolkata, Mohanpur 741246, West Bengal, India;1. Eskisehir Osmangazi University, Department of Geological Engineering, 26040 Eskisehir, Turkey;2. Department of Earth Sciences, Royal Holloway University of London, Egham TW20 0EX, UK;3. Department of Earth Sciences, Durham University, Durham DH1 3LE, UK |
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| Abstract: | Active faults at a range in scales are observed in different directions (E-W, N-S and NE-SW) in the extensional tectonic regime of the Aegean region, western Turkey. However, mechanisms and types of faults in the Gulf of Izmir have not been investigated properly. Tectonic setting in the gulf together with the origin and characteristics of faults were studied in this study by integrating interpretation from various very high resolution acoustic data (multibeam bathymetry and CHIRP very high resolution seismic) acquired in the Gulf of Izmir.The Gulf of Izmir has thick, unconsolidated, stratified sediment cover. The water depth increases from the inner part (SE) to the outer part (NW) of the gulf with complex sea floor morphology. However, northeastern part of the coastal region is very shallow because of the sedimentary influx transported by the Gediz River. The western margin and the southern part of the gulf were formed under the influence of Uzunada (Uzun Island) and Izmir Faults, respectively. In the southern offshore, there is only one, E-W directional normal fault dipping through the north and corresponding to the offshore segment of the Izmir Fault Zone to the west. The acoustic data enable identification of the Uzunada Fault Zone extending as a simple lineament from near Guzelbahce in the south but bifurcating toward the NE of the Cicek Archipelago and terminating with left-lateral slip in the E-NE of the Hekim Island. After the sinistral strike-slip, the fault re-extends in the NW direction untill the mid of Uzunada as a single fault segment. Then, the fault is observed as a bunch of many active fault segments (like horse-tail splays) to the east of Uzunada with N-NW elongation through the outer gulf. These segments were chronologically succeeded from the east to the west. This progradational pattern is attributed to westward extension of the Gulf of Izmir with anti-clockwise rotational escape of the Anatolian Plate. In addition, progradation of faults was controlled by the NE-SW directional tear faults which may have played a key role in the shoreline extension and general pattern of the outer gulf islands. A very young graben in the central part of the gulf, also dislocated by the tear faults was observed parallel to the Uzunada Fault Zone as another indicator of ongoing fan-shaped opening of the gulf. These tectonic elements are consistent with earlier interpretation of GPS-based observations indicating a four-wheel gear system of rigid-body rotations. Additionally, a new fault extending from the far offshore of Foca to Suzbeyli village to the south was identified in this study. Its NW-SE extension is angular to the previous tectonic elements. All these elements apparently project at least 10 km farther northward, in the offshore Foca where the earthquake epicenters cluster. |
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| Keywords: | Uzunada Fault Zone Izmir Fault Zone Izmir Central Graben Very high resolution seismic Multibeam data |
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