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Title: A glance at velocity structure of Izmir

Journal Article · · AIP Conference Proceedings
DOI:https://doi.org/10.1063/1.4945833· OSTI ID:22591183
 [1];  [1]
  1. Dokuz Eylul University, Faculty of Engineering, Geophysical Engineering Department, Izmir (Turkey)

In this study; we investigated velocity structure of Izmir and surroundings. We used local earthquake data which was recorded by different type of instruments and obtained high resolution 3D sections. We selected more than 400 earthquakes which were occurred between 2010 and 2013. Examined tomographic sections especially in Izmir along coastal areas (Mavisehir-Inciraltı); revealed the low speed zone. Along this low-speed zone; it is consistent with the results obtained from the stratigraphic section and surface geology. While; low velocity zones are associated with faults and water content; high velocity is related to magmatic rocks or compact rocks. Along Karsıyaka, Seferihisar, Orhanlı, Izmir fault zones; low P velocity was observed. When examined higher elevations of the topography; which are composed of soured magmatic material is dominated by high P velocity. In all horizontal sections; resolution decreasing with increasing depth. The reason for this; the reduction of earthquakes causes ray tracing problems.

OSTI ID:
22591183
Journal Information:
AIP Conference Proceedings, Vol. 1726, Issue 1; Conference: ICANAS 2016: International conference on advances in natural and applied sciences, Antalya (Turkey), 21-23 Apr 2016; Other Information: (c) 2016 Author(s); Country of input: International Atomic Energy Agency (IAEA); ISSN 0094-243X
Country of Publication:
United States
Language:
English