1 Ocak 2016 Dergi makalesi Açık Erişim

Brogi, Andrea; Alcicek, M. Cihat; Yalciner, Cahit Caglar; Capezzuoli, Enrico; Liotta, Domenico; Meccheri, Marco; Rimondi, Valentina; Ruggieri, Giovanni; Gandin, Anna; Boschi, Chiara; Buyuksarac, Aydin; Alcicek, Hulya; Bulbul, Ali; Baykara, Mehmet Oruc; Shen, Chuan-Chou

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    "creators": [
      {
        "affiliation": "Univ Bari, Dept Earth & Geoenvironm Sci, I-70125 Bari, Italy", 
        "name": "Brogi, Andrea"
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      {
        "affiliation": "Univ Pamukkale, Dept Geol, TR-20070 Denizli, Turkey", 
        "name": "Alcicek, M. Cihat"
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      {
        "affiliation": "Canakkale Onsekiz Mart Univ, Can Vocat Coll, TR-17400 Canakkale, Turkey", 
        "name": "Yalciner, Cahit Caglar"
      }, 
      {
        "affiliation": "Univ Perugia, Dept Phys & Geol, I-06123 Perugia, Italy", 
        "name": "Capezzuoli, Enrico"
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      {
        "affiliation": "Univ Bari, Dept Earth & Geoenvironm Sci, I-70125 Bari, Italy", 
        "name": "Liotta, Domenico"
      }, 
      {
        "affiliation": "Univ Siena, Dept Phys Earth & Environm Sci, I-53100 Siena, Italy", 
        "name": "Meccheri, Marco"
      }, 
      {
        "affiliation": "IGG CNR, Inst Geosci & Earth Resources, Via G La Pira 4, I-50121 Florence, Italy", 
        "name": "Rimondi, Valentina"
      }, 
      {
        "affiliation": "IGG CNR, Inst Geosci & Earth Resources, Via G La Pira 4, I-50121 Florence, Italy", 
        "name": "Ruggieri, Giovanni"
      }, 
      {
        "affiliation": "Univ Siena, Dept Phys Earth & Environm Sci, I-53100 Siena, Italy", 
        "name": "Gandin, Anna"
      }, 
      {
        "affiliation": "IGG CNR, Inst Geosci & Earth Resources, Via G Moruzzi 1, I-56124 Pisa, Italy", 
        "name": "Boschi, Chiara"
      }, 
      {
        "affiliation": "Bitlis Eren Univ, Dept Civil Engn, TR-13000 Bitlis, Turkey", 
        "name": "Buyuksarac, Aydin"
      }, 
      {
        "affiliation": "Univ Pamukkale, Dept Geol, TR-20070 Denizli, Turkey", 
        "name": "Alcicek, Hulya"
      }, 
      {
        "affiliation": "Univ Pamukkale, Dept Geol, TR-20070 Denizli, Turkey", 
        "name": "Bulbul, Ali"
      }, 
      {
        "name": "Baykara, Mehmet Oruc"
      }, 
      {
        "affiliation": "Natl Taiwan Univ, Dept Geosci, High Precis Mass Spectrometry & Environm Change L, Taipei 106, Taiwan", 
        "name": "Shen, Chuan-Chou"
      }
    ], 
    "description": "Coexistence of thermal springs, travertine deposits and tectonic activity is a recurring feature for most geothermal areas. Although such a certainty, their relationships are debated mainly addressing on the role of the tectonic activity in triggering and controlling fluids flow and travertine deposition. In this paper, we present the results of an integrated study carried out in a geothermal area located in western Anatolia (Turkey), nearby the well-known Pamukkale area (Denizli Basin). Our study focused on the relationships among hydrothermal fluids circulation, travertine deposition and tectonic activity, with particular emphasis on the role of faults in controlling fluids upwelling, thermal springs location and deposition of travertine masses. New field mapping and structural/kinematics analyses allowed us to recognize two main faults systems (NW- and NE-trending), framed in the Neogene-Quaternary extensional tectonic evolution of western Anatolia. A geo-radar (GPR) prospection was also provided in a key-area, permitting us to reconstruct a buried fault zone and its relationships with the development of a fissure-ridge travertine deposit (Kamara fissure-ridge). The integration among structural and geophysical studies, fluids inclusion, geochemical, isotopic data and Th-230/U-238 radiometric age determination on travertine deposits, depict the characteristics of the geothermal fluids and their pathway, up to the surface. Hydrological and seismological data have been also taken in account to investigate the relation between local seismicity and fluid upwelling. As a main conclusion we found strict relationships among tectonic activity, earthquakes occurrence, and variation of the physical/chemical features of the hydrothermal fluids, presently exploited at depth, or flowing out in thermal springs. In the same way, we underline the tectonic role in controlling the travertine deposition, making travertine (mainly banded travertine) a useful proxy to reconstruct the seismological history of an area, as well as the characteristics of the parent geothermal fluids, adding an effective tool for geothermal exploration tasks. (C) 2016 Elsevier B.V. All rights reserved.", 
    "doi": "10.1016/j.tecto.2016.05.003", 
    "has_grant": false, 
    "journal": {
      "pages": "211-232", 
      "title": "TECTONOPHYSICS", 
      "volume": "680"
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    "license": {
      "id": "cc-by"
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    "publication_date": "2016-01-01", 
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    "title": "Hydrothermal fluids circulation and travertine deposition in an active tectonic setting: Insights from the Kamara geothermal area (western Anatolia, Turkey)"
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