Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia)
Аутори
Batoćanin, NatalijaWróblewski, Wojciech
Carević, Ivana
Durlević, Uroš
Gajić, Violeta
Valjarević, Aleksandar
Чланак у часопису (Објављена верзија)
Метаподаци
Приказ свих података о документуАпстракт
Tufa accumulations from the Gostilje River Basin and the Sopotnica River Basin in SW Serbia are represented by both active and fossil tufa precipitates. The aim of this study is to distinguish and describe different tufa facies and to determine the environmental conditions, based on stable isotope data. We also compare our analysis with other tufa deposits in Europe. Four facies are distinguished: moss tufa, algal tufa, stromatolitic laminated tufa, and phytoclastic tufa. The dominant constituent of all tufa samples is low Mg-calcite, whereas the presence of sylvite is noted in two samples from the Gostilje River Basin. The δ18O values range from −9.07‰ to −10.79‰ (mean value: −9.81‰), while the δ13C values range from −6.50‰ to −10.34‰ (mean values −9.01‰). The stable isotope values (δ13C and δ18O) indicate that these tufa deposits were precipitated from cold, ambient water supported by CO2 of an atmospheric origin. We emphasize that this is the first data about stable isotope analyses... of tufa deposits from Serbia.
Кључне речи:
tufa / facies / stable isotopes / Sopotnica River Basin / Gostilje River Basin / SerbiaИзвор:
Applied Sciences, 2023, 13, 5, 3190-Издавач:
- Basel : MDPI
Финансирање / пројекти:
- Министарство науке, технолошког развоја и иновација Републике Србије, институционално финансирање - 200091 (Универзитет у Београду, Географски факултет) (RS-200091)
- Министарство науке, технолошког развоја и иновација Републике Србије, институционално финансирање - 200126 (Универзитет у Београду, Рударско-геолошки факултет) (RS-200126)
Колекције
Институција/група
Geografski fakultetTY - JOUR AU - Batoćanin, Natalija AU - Wróblewski, Wojciech AU - Carević, Ivana AU - Durlević, Uroš AU - Gajić, Violeta AU - Valjarević, Aleksandar PY - 2023 UR - http://gery.gef.bg.ac.rs/handle/123456789/1187 AB - Tufa accumulations from the Gostilje River Basin and the Sopotnica River Basin in SW Serbia are represented by both active and fossil tufa precipitates. The aim of this study is to distinguish and describe different tufa facies and to determine the environmental conditions, based on stable isotope data. We also compare our analysis with other tufa deposits in Europe. Four facies are distinguished: moss tufa, algal tufa, stromatolitic laminated tufa, and phytoclastic tufa. The dominant constituent of all tufa samples is low Mg-calcite, whereas the presence of sylvite is noted in two samples from the Gostilje River Basin. The δ18O values range from −9.07‰ to −10.79‰ (mean value: −9.81‰), while the δ13C values range from −6.50‰ to −10.34‰ (mean values −9.01‰). The stable isotope values (δ13C and δ18O) indicate that these tufa deposits were precipitated from cold, ambient water supported by CO2 of an atmospheric origin. We emphasize that this is the first data about stable isotope analyses of tufa deposits from Serbia. PB - Basel : MDPI T2 - Applied Sciences T1 - Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia) VL - 13 IS - 5 SP - 3190 DO - 10.3390/app13053190 ER -
@article{ author = "Batoćanin, Natalija and Wróblewski, Wojciech and Carević, Ivana and Durlević, Uroš and Gajić, Violeta and Valjarević, Aleksandar", year = "2023", abstract = "Tufa accumulations from the Gostilje River Basin and the Sopotnica River Basin in SW Serbia are represented by both active and fossil tufa precipitates. The aim of this study is to distinguish and describe different tufa facies and to determine the environmental conditions, based on stable isotope data. We also compare our analysis with other tufa deposits in Europe. Four facies are distinguished: moss tufa, algal tufa, stromatolitic laminated tufa, and phytoclastic tufa. The dominant constituent of all tufa samples is low Mg-calcite, whereas the presence of sylvite is noted in two samples from the Gostilje River Basin. The δ18O values range from −9.07‰ to −10.79‰ (mean value: −9.81‰), while the δ13C values range from −6.50‰ to −10.34‰ (mean values −9.01‰). The stable isotope values (δ13C and δ18O) indicate that these tufa deposits were precipitated from cold, ambient water supported by CO2 of an atmospheric origin. We emphasize that this is the first data about stable isotope analyses of tufa deposits from Serbia.", publisher = "Basel : MDPI", journal = "Applied Sciences", title = "Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia)", volume = "13", number = "5", pages = "3190", doi = "10.3390/app13053190" }
Batoćanin, N., Wróblewski, W., Carević, I., Durlević, U., Gajić, V.,& Valjarević, A.. (2023). Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia). in Applied Sciences Basel : MDPI., 13(5), 3190. https://doi.org/10.3390/app13053190
Batoćanin N, Wróblewski W, Carević I, Durlević U, Gajić V, Valjarević A. Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia). in Applied Sciences. 2023;13(5):3190. doi:10.3390/app13053190 .
Batoćanin, Natalija, Wróblewski, Wojciech, Carević, Ivana, Durlević, Uroš, Gajić, Violeta, Valjarević, Aleksandar, "Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia)" in Applied Sciences, 13, no. 5 (2023):3190, https://doi.org/10.3390/app13053190 . .