Hydrothermal Fluids Circulation And Travertine Deposition In An Active Tectonic Setting: Insights From The Kamara Geothermal Area (Western Anatolia, Turkey)

Autor: Brogi A.[1], Alçiçek M.C.[2], Yalçiner C.T.[3], Capezzuoli E.[4], Liotta D. [1, Meccheri M.[5], Rimondi V.[6], Ruggieri G.[7], Gandin A.[5], Boschi C.[7], Büyüksarac A.[8], Alçiçek H.[2], Bülbül A.[2], Baykara M.O.[2, Shen C.-C. [9]

Publikováno v: Tectonophysics (Amst. Online) 680 (2016): 211–232. doi:10.1016/j.tecto.2016.05.003
info:cnr-pdr/source/autori:Brogi A.[1], Alçiçek M.C.[2], Yalçiner C.T.[3], Capezzuoli E.[4], Liotta D. [1,6], Meccheri M.[5], Rimondi V.[6], Ruggieri G.[7], Gandin A.[5], Boschi C.[7], Büyüksarac A.[8], Alçiçek H.[2], Bülbül A.[2], Baykara M.O.[2,9], Shen C.-C. [9]/titolo:Hydrothermal fluids circulation and travertine deposition in an active tectonic setting: Insights from the Kamara geothermal area (western Anatolia, Turkey)/doi:10.1016%2Fj.tecto.2016.05.003/rivista:Tectonophysics (Amst. Online)/anno:2016/pagina_da:211/pagina_a:232/intervallo_pagine:211–232/volume:680

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 triggerin

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