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dc.contributor.authorBrogi, Andrea
dc.contributor.authorAlcicek, M. Cihat
dc.contributor.authorYalciner, Cahit Caglar
dc.contributor.authorCapezzuoli, Enrico
dc.contributor.authorLiotta, Domenico
dc.contributor.authorMeccheri, Marco
dc.contributor.authorRimondi, Valentina
dc.contributor.authorRuggieri, Giovanni
dc.date.accessioned16/12/21 12:07
dc.date.available16/12/21 12:07
dc.date.issued2016
dc.identifier.issn0040-1951
dc.identifier.urihttp://dspace.beu.edu.tr:8080/xmlui/handle/20.500.12643/10467
dc.identifier.urihttps://doi.org/10.1016/j.tecto.2016.05.003
dc.description.abstractCoexistence 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
dc.description.sponsorshipTUBITAK (Scientific and Techological Research Council of Turkey)Turkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK) [113Y551]; CNR (National Research Council of Italy)Consiglio Nazionale delle Ricerche (CNR) [113Y551]
dc.language.isoEnglish
dc.publisherElsevıer
dc.sourceTectonophysıcs
dc.titleHydrothermal fluids circulation and travertine deposition in an active tectonic setting: Insights from the Kamara geothermal area (western Anatolia, Turkey)
dc.typeArticle
dc.identifier.startpage211
dc.identifier.endpage232
dc.identifier.doi10.1016/j.tecto.2016.05.003
dc.identifier.wosWOS:000379277000015
dc.identifier.volume680


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