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Temporal changes in geochemical-isotopic systematics of the late Pleistocene Akkaya travertines (Turkey) - Implications for fluid flow circulation and seismicity

Yildirim, Gokhan; Mutlu, Halim; Karabacak, Volkan; Uysal, I. Tonguc; Dirik, Kadir; Temel, Abidin; Yuce, Galip; Zhao, Jian-xin


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        "affiliation": "Ankara Univ, Geol Engn Dept, Ankara, Turkey", 
        "name": "Yildirim, Gokhan"
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      {
        "affiliation": "Ankara Univ, Geol Engn Dept, Ankara, Turkey", 
        "name": "Mutlu, Halim"
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      {
        "affiliation": "Eskisehir Osmangazi Univ, Geol Engn Dept, Eskisehir, Turkey", 
        "name": "Karabacak, Volkan"
      }, 
      {
        "affiliation": "Ankara Univ, Geol Engn Dept, Ankara, Turkey", 
        "name": "Uysal, I. Tonguc"
      }, 
      {
        "affiliation": "Hacettepe Univ, Geol Engn Dept, Ankara, Turkey", 
        "name": "Dirik, Kadir"
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      {
        "affiliation": "Hacettepe Univ, Geol Engn Dept, Ankara, Turkey", 
        "name": "Temel, Abidin"
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      {
        "affiliation": "Hacettepe Univ, Geol Engn Dept, Ankara, Turkey", 
        "name": "Yuce, Galip"
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      {
        "affiliation": "Univ Queensland, Sch Earth & Environm Sci, Radiogen Isotope Facil, Brisbane, Qld, Australia", 
        "name": "Zhao, Jian-xin"
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    "description": "We investigate the temporal variations in stable carbon and oxygen and radiogenic Sr isotope as well as rare earth element contents of Akkaya travertine deposits in the Eskipazar region, northwest Turkey. U-Th age data indicate that studied travertines in the periphery of the 1944-earthquake rupture of the North Anatolian Fault Zone formed in a time span of 93 to 1.8 ka BP. The younger group is represented by fissure-filling carbonates whereas the older sequence is composed of veins with varying crystallization ages that are injected to bedded travertines. The age data on vein injections and fissure-ridge travertines in the Akkaya site indicate the seismic reactivation along the west-central part of the North Anatolian Fault Zone to be intensified at least 4 periods (1.8, 20, 47 and 88 ka BP) during the last 90 ka.", 
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    "title": "Temporal changes in geochemical-isotopic systematics of the late Pleistocene Akkaya travertines (Turkey) - Implications for fluid flow circulation and seismicity"
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