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| | Abstract | | Eskisehir, Turkey, which is formed by sedimentary deposits, has potentially moderate seismic risk by active faults, in the north-eastern area of Turkey. The city of Eskisehir has been widely developing in the sedimentary basin and therefore, buildings located in Eskisehir have several types of ground motions affected by the local site effects during earthquakes. In this report, we performed microtremors observations on buildings and estimated normal mode of buildings for total 28 buildings located in Eskisehir, Turkey. |
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