1 Ocak 2021 Dergi makalesi Açık Erişim

Ozmen, Ozgur Tuna; Yamanaka, Hiroaki; Ates, Erkan; Tekin, Kudret; Ceken, Ulubey; Koparmal, Erkan; Etiz, Ali; Elmas, Nalan

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        "affiliation": "Turkish AFAD, Prime Minist Disaster & Emergency Management Auth, Ankara, Turkey", 
        "name": "Ozmen, Ozgur Tuna"
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      {
        "affiliation": "Tokyo Inst Technol, Dept Architecture & Bldg Engn, Tokyo, Japan", 
        "name": "Yamanaka, Hiroaki"
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      {
        "affiliation": "Turkish AFAD, Prime Minist Disaster & Emergency Management Auth, Ankara, Turkey", 
        "name": "Ates, Erkan"
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      {
        "affiliation": "Turkish AFAD, Prime Minist Disaster & Emergency Management Auth, Ankara, Turkey", 
        "name": "Tekin, Kudret"
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      {
        "affiliation": "Turkish AFAD, Prime Minist Disaster & Emergency Management Auth, Ankara, Turkey", 
        "name": "Ceken, Ulubey"
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      {
        "affiliation": "Prime Minist, Econ Social & Cultural Affairs Dept, Ankara, Turkey", 
        "name": "Koparmal, Erkan"
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      {
        "affiliation": "Denizli Prov Directorate Disaster & Emergency, Denizli, Turkey", 
        "name": "Etiz, Ali"
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      {
        "affiliation": "Aydin Prov Directorate Disaster & Emergency, Aydin, Turkey", 
        "name": "Elmas, Nalan"
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    "description": "This paper reports the results of a case study of the application of the microtremor exploration method in western Turkey. We have conducted microtremor surveys at strong motion stations in Aydin and Denizli provinces to derive shallow S-wave velocity profiles. Array records of vertical microtremor motion were acquired at 12 and 15 stations in Aydin and Denizli provinces, respectively. A spatial autocorrelation analysis was applied to the records to estimate Rayleigh wave phase velocities in the frequency range of 3-30 Hz. Then, the phase velocity dispersion at each station was inverted to a one-dimensional S-wave profile down to a maximum depth of about 50 m. The soil models at 5 and 11 stations in Aydin and Denizli provinces, respectively, have a bedrock with an S-wave velocity of 400-600 m/s at depths less than 10 m. The spatial distribution of average S-wave velocities in the top 30 m of the revealed profiles shows low values in the Buyuk Menderes Graben and the Denizli Basin, and high values in the surrounding hill or mountain areas. We compared our S-wave profiles with those from previous surface-wave studies. S-wave velocities in shallow parts to a depth of 5-10 m are similar in the two studies. However, S-wave velocities in deep parts are different at some of the stations.", 
    "doi": "10.1080/08123985.2021.1880269", 
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      "issue": "6", 
      "pages": "659-668", 
      "title": "EXPLORATION GEOPHYSICS", 
      "volume": "52"
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    "science_branches": [
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    "title": "Microtremor exploration at strong motion stations in Aydin and Denizli provinces, western Turkey"
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