Evidence of microbiologic activity in modern travertines: Sicakcermik geothermal field, central Turkey

Modern travertine deposits are observed in the Sicakçermik hot springs located northwest of Sivas, central Anatolia. They are the carbonate deposits of crustal (spongy) and/or alabaster-textured formations controlled by both organic and inorganic processes. The structures formed under the influence...

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Veröffentlicht in:Carbonates and evaporites 2000-01, Vol.15 (1), p.18-27
Hauptverfasser: Tekin, Erdogan, Kayabali, Kamil, Ayyildiz, Turhan, Ileri, Ozden
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Sprache:eng
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