Calcite veining and feeding conduits in a hydrothermal system: Insights from a natural section across the Pleistocene Gölemezli travertine depositional system (western Anatolia, Turkey)

Autor: Capezzuoli E.[1], Ruggieri G.[2], Rimondi V.[2, Brogi A.[4], Liotta D. [4, Alcicek M.[6], Alcicek H.[6], Bulbul A.[6], Gandin A.[7], Meccheri M.[8], Shen C.[9], Baykara M. [6

Publikováno v: Sedimentary Geology 364 (2018): 180–203. doi:10.1016/j.sedgeo.2017.12.012
info:cnr-pdr/source/autori:Capezzuoli E.[1], Ruggieri G.[2], Rimondi V.[2,3], Brogi A.[4], Liotta D. [4,5], Alcicek M.[6], Alcicek H.[6], Bulbul A.[6], Gandin A.[7], Meccheri M.[8], Shen C.[9], Baykara M. [6,8]/titolo:Calcite veining and feeding conduits in a hydrothermal system: Insights from a natural section across the Pleistocene Golemezli travertine depositional system (western Anatolia, Turkey)/doi:10.1016%2Fj.sedgeo.2017.12.012/rivista:Sedimentary Geology/anno:2018/pagina_da:180/pagina_a:203/intervallo_pagine:180–203/volume:364
Università degli studi di Firenze-IRIS

Linking the architecture of structural conduits with the hydrothermal fluids migrating from the reservoir up to the surface is a key-factor in geothermal research. A contribution to this achievement derives from the study of spring-related travertine

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::696f546238756cc039b7bdc357071368
https://hdl.handle.net/11499/10859