engleski

Yenice travertines, Kamara hot spring fissure ridge and Guney waterfall tufa

Isotope analyses of 14C activity/age and d13C and d18O composition of 19 tufa samples collected at the sites described above were performed. The recent tufa samples (fresh carbonate precipitated in the water) showed 14C activity from 63.8 to 70.6 pMC (percent of modern carbon), with increasing 14C activity downstream (Güney site). The 14C ages of old/dry tufa deposits showed that they were formed in the Holocene.

travertine; tufa; Denizli

Predavanje je održano u okviru Field trip organiziranog u okviru 1. International Travertine Symposium, Denizli, Turska.