1 Ocak 2021 Dergi makalesi Açık Erişim

Erginal, Ahmet Evren; Erenoglu, Ramazan Cuneyt; Yildirim, Cengiz; Selim, H. Haluk; Kiyak, Nafiye Gunec; Erenoglu, Oya; Ulugergerli, Emin; Karabiyikoglu, Mustafa

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        "affiliation": "Canakkale Onsekiz Mart Univ, Fac Educ, Dept Geog Educ, TR-17100 Canakkale, Turkey", 
        "name": "Erginal, Ahmet Evren"
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      {
        "affiliation": "Canakkale Onsekiz Mart Univ, Fac Engn, Dept Geomat Engn, TR-17100 Canakkale, Turkey", 
        "name": "Erenoglu, Ramazan Cuneyt"
      }, 
      {
        "affiliation": "Istanbul Tech Univ, Eurasia Inst Earth Sci, TR-34469 Istanbul, Turkey", 
        "name": "Yildirim, Cengiz"
      }, 
      {
        "affiliation": "Istanbul Gelisim Univ, Dept Civil Engn, TR-34310 Istanbul, Turkey", 
        "name": "Selim, H. Haluk"
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      {
        "affiliation": "Istanbul OSLAB Res & Archeometry Grp, Istanbul, Turkey", 
        "name": "Kiyak, Nafiye Gunec"
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      {
        "affiliation": "Canakkale Onsekiz Mart Univ, Fac Educ, Dept Geog Educ, TR-17100 Canakkale, Turkey", 
        "name": "Erenoglu, Oya"
      }, 
      {
        "affiliation": "Canakkale Onsekiz Mart Univ, Fac Engn, Dept Geophys Engn, TR-17100 Canakkale, Turkey", 
        "name": "Ulugergerli, Emin"
      }, 
      {
        "affiliation": "Ardahan Univ, Fac Humanities & Letters, Dept Geog, TR-75000 Ardahan, Turkey", 
        "name": "Karabiyikoglu, Mustafa"
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    "description": "A historical earthquake-related co-seismic deformation observed on beachrock beds along the southern shoreline of Lake Iznik is discussed as a new paleoseismic record for an 8th century AD earthquake in the Middle Strand of the North Anatolian Fault, NW Turkey. Electrical Resistivity Tomography (ERT) images beneath the beachrock surface allowed monitoring of the subsurface trace of a normal fault dipping north along a 100 m surface rupture. No strike-slip deformation exists along the rupture, suggesting that the deformation in the beachrock is connected with a secondary structure, and that the main surface rupture was under the lake waters. The deformed beds of the beachrock, dated using Optically Stimulated Luminescence (OSL) to 1.3 +/- 0.15 ka, are overlain by an undeformed secondary deposition of beds dated to 1.2 +/- 0.09 ka. This allows us to narrow down the time of the faulting and implying that it was most likely a result of the AD 715 earthquake.", 
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      "title": "TECTONOPHYSICS", 
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    "title": "Co-seismic beachrock deformation of 8th century AD Earthquake in Middle Strand of North Anatolian Fault, Lake Iznik, NW Turkey"
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