Quaternary to Recent travertines in the Denizli basin are distinguished in 9 lithofacies according to the field and microscopic features. These are: 1) Crystalline crust, 2) Shrub, 3) Pisolith, 4) Paper-thin raft, 5) Coated gas bubble, 6) Reed, 7) Lithoclast, 8) Pebbly travertines and 9) Palaeosols. Various combinations of the distinguished lithofacies are deposited on the slope, depression, mound, fissure ridge and channel depositional environments. In addition, these main depositional environments are divided into subenvironments. As to isotope analysis made of some travertine samples, d3C and d8O values show a wide distribution. The d13C values are between 0.35%o and 6.70%o; d18O values are -6.47%o to -15.10 %o. Consequently, an isotopic grouping has been brought up based on lithofacies variation and depositional environments.
Primary Language | English |
---|---|
Subjects | Engineering |
Journal Section | Articles |
Authors | |
Publication Date | June 1, 2002 |
Published in Issue | Year 2002 Volume: 125 Issue: 125 |
Copyright and Licence
The Bulletin of Mineral Research and Exploration keeps the Law on Intellectual and Artistic Works No: 5846. The Bulletin of Mineral Research and Exploration publishes the articles under the terms of “Creatice Common Attribution-NonCommercial-NoDerivs (CC-BY-NC-ND 4.0)” licence which allows to others to download your works and share them with others as long as they credit you, but they can’t change them in any way or use them commercially.
For further details;
https://creativecommons.org/licenses/?lang=en