Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.13091/759
Title: Subdividing the tectonic elements of Aegean and Eastern Mediterranean with gravity and GPS data
Authors: Kahveci, Muzaffer
Çırmık, Ayça
Doğru, Fikret
Pamukçu, Oya
Gönenç, Tolga
Keywords: Gps
Tectonic Elements
Wgm2012 Model
Gravity
Western Anatolia
Eastern Mediterranean
Aegean Sea
Evolution
Deformation
Plate
Constraints
Kinematics
Extension
System
Strain
Trench
Greece
Issue Date: 2019
Publisher: SPRINGER INTERNATIONAL PUBLISHING AG
Abstract: Western Anatolia has been formed by the motions of the African plate, Arabian plate and Hellenic Subduction zone. The Hellenic Subduction zone, which has high seismicity, is the main tectonic feature of the eastern Mediterranean Sea related to the subduction of the African Plate beneath the Aegean Sea Plate. The Hellenic Subduction zone has a complex lithospheric structure and shows complex differences in the Aegean Sea in terms of continental crust thickness and mantle velocity. In the study area, the directions of Global Positioning System (GPS) velocity vectors which are towards SE change towards S from North of Western Anatolia to Hellenic Subduction zone. It is thought that the factor which controls this mechanism is the shear force or subduction zone located in Aegean Sea. Western Anatolia region, which is located in Western Anatolia Extensional province, includes several morphologically significant N-S trending active normal faults. Besides, the NE-SW and NW-SE trending faults, which their kinematic features change from north to south, are very effective on the tectonic regime of the region. Additionally, for determining the boundaries of these tectonic elements, the Complete Spherical Bouguer (CSB) gravity anomaly of study area was calculated by using World Gravity Map (WGM2012) model. Moreover, in historical and instrumental studies, the high seismicity of the study area is remarkable. It is thought that this case is also related with the mechanism which oriented the GPS velocity vectors to southward. Consequently, the dominant kinematic structure of the region was classified by combining the GPS velocity vectors computed for Izmir and its surroundings bounded by Western Anatolia, Aegean Sea and Eastern Mediterranean and the CSB gravity anomaly. Finally, the results were interpreted together with focal depth distributions of earthquakes and Bouguer gravity data.
URI: https://doi.org/10.1007/s11600-019-00270-w
https://hdl.handle.net/20.500.13091/759
ISSN: 1895-6572
1895-7455
Appears in Collections:Mühendislik ve Doğa Bilimleri Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collections
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collections

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