GPS-derived velocity field of the Iznik-Mekece segment of the North Anatolian Fault Zone

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• 作者：Haluk Ozener ^{ozener@boun.edu.tr} ; Onur Yilmaz ; ^{onur.yilmaz@boun.edu.tr} ; Asli Dogru ^{asli.dogru@boun.edu.tr} ; Bulent Turgut ^{turgut@boun.edu.tr} ; Onur Gurkan ^{gurkano@boun.edu.tr}
• 关键词：North Anatolian Fault Zone ; Iznik-Mekece Segment ; GPS ; Tectonics ; Deformation
• 刊名：Journal of Geodynamics
• 出版年：2013
• 出版时间：July, 2013
• 年：2013
• 卷：67
• 期：Complete
• 页码：46-52
• 全文大小：1666 K

文摘

Space-based tectonic studies on the western part of the North Anatolian Fault Zone (NAFZ) have been conducted over two decades. After the August 17, 1999, Izmit earthquake (M_w = 7.4), this region attracted greater scientific interest, and the collected data became more valuable. The Geodesy Department of the Kandilli Observatory and Earthquake Research Institute (KOERI) at Bogazici University established three micro-geodetic networks to the east of Akyazi, east of Iznik, and west of Lake Sapanca in the eastern part of the Marmara region; GPS data have been continually collected at these locations since 1994. The NAFZ branches out in the western part of the Marmara region and extends up to the Aegean Sea. Segments of the fault passing through the Marmara Sea are considered active, and this has increased concern regarding imminent earthquakes. Conventional geodetic measurements made between 1990 and 1994 are not sufficient for monitoring small movements. However, GPS has played a very important role in detecting such deformations in the area after 1994. The Iznik network, with 10 points, is bilaterally located on the Iznik-Mekece fault. Six years of GPS data for 2004-2010 collected for the monitoring of crustal deformation showed that the Iznik-Mekece fault segment moves westward at about 22 ¡À 1 mm/yr with respect to the Eurasia fixed reference frame. The GPS observations show that there is no strain accumulation in the area.