Investigations on Northern Urmia-Dokhtar travertines and comparison with north Sanandaj-Sirjan travertines using 18O and 13C stable isotopes

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

Roshanak r.; ZARASVANDI A.R.; POURKASEB H.; Moore Farid

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2018 | Volume:27 | Issue:106 Page(s): 143-152

Download Full-Text

Persian Verion

View:

632

Download:

Cites:

Information Journal Paper

Title

Investigations on Northern Urmia-Dokhtar travertines and comparison with north Sanandaj-Sirjan travertines using 18O and 13C stable isotopes

Author(s)

Roshanak r. | ZARASVANDI A.R. | POURKASEB H. | Moore Farid | Issue Writer Certificate

Keywords

TravertineQ2

Urmia-DokhtarQ1

Sanandaj-SirjanQ1

18O and 13C IsotopesQ1

Abstract

Main Travertines of Iran are located in a NW-SE trending belt (Urmia-Dokhtar Belt), extending from Tabriz to Zahedan. Neo-tectonic activities (Plecene to now) with Travertine deposits around hot springs and volcanic features can be seen along this belt. In this study, East Azerbaijan Travertines (northern of Urmia-Dokhtar structural zone) is investigated and are compared with Kurdistan and West Azerbaijan Travertine (northern of Sanandaj-Sirjan structural zone). The studied samples classify in thermogene category, using geochemical, mineralogical and 18O and 13C Isotopes studies. Based on facies studies, northern Urmia-Dokhtar Travertines fall in oncoid crystalline while Sanandaj-Sirjan Travertines show oncoid, crystalline crust and pebbly facies. Using the measured δ 13C values of Travertine gives the δ 13C of the CO2 released from the water during Travertine deposition. Source of the CO2 in the water springs was crustal magmatic water. The stable isotope composition of two areas were compared with Turkey Travertines and they show similar genesis, CO2 source and isotopic composition.

Cites

No record.

References

No record.

Cite

APA: Copy

Roshanak, r., ZARASVANDI, A.R., POURKASEB, H., & Moore, Farid. (2018). Investigations on Northern Urmia-Dokhtar travertines and comparison with north Sanandaj-Sirjan travertines using 18O and 13C stable isotopes. GEOSCIENCES, 27(106 ), 143-152. SID. https://sid.ir/paper/32107/en

Vancouver: Copy

Roshanak r., ZARASVANDI A.R., POURKASEB H., Moore Farid. Investigations on Northern Urmia-Dokhtar travertines and comparison with north Sanandaj-Sirjan travertines using 18O and 13C stable isotopes. GEOSCIENCES[Internet]. 2018;27(106 ):143-152. Available from: https://sid.ir/paper/32107/en

IEEE: Copy

r. Roshanak, A.R. ZARASVANDI, H. POURKASEB, and Farid Moore, “Investigations on Northern Urmia-Dokhtar travertines and comparison with north Sanandaj-Sirjan travertines using 18O and 13C stable isotopes,” GEOSCIENCES, vol. 27, no. 106 , pp. 143–152, 2018, [Online]. Available: https://sid.ir/paper/32107/en

Related Journal Papers