Structural controls on the hydrogeochemistry of Azarshahr travertine springs, NW Iran

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.

TAGHIPOUR K.; KHATIB M.M.; HEYHAT M.R.; VAEZI HIR A.R.; SHABANIAN E.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Geology Year:2020 | Volume:13 | Issue:52 Page(s): 105-122

Download Full-Text

Persian Verion

View:

618

Download:

Cites:

Information Journal Paper

Title

Structural controls on the hydrogeochemistry of Azarshahr travertine springs, NW Iran

Author(s)

Keywords

Travertine springsQ1

Structural controlsQ1

HydrogeochemistryQ2

Urmia LakeQ2

Abstract

Travertine deposits in Azarshahr, NW Iran, are one of the most extensive travertine deposits in the world. The process of travertine deposit is currently active in the several springs. It was used a multidisciplinary approach to determine the source of fluids and structural characteristics of Travertine springs. Results of in-situ measurements and type of travertine deposits, demonstrate that the springs are of thermogenic type with hydrothermal sources. Hydrogeochemical diagrams and ionic ratios represent that the type of spring waters are calcium carbonate, with increased sodium and chloride ions levels due to mixing with brine waters. Geophysical studies showed that these brines originated from the Urmia Lake or related brines, which are intruded through fracture systems to relay zones of faults and mixed with hydrothermal bicarbonate-saturated fluids. This phenomenon shows that hydrochemistry of Travertine springs are affected by Urmia Lake or related brines.

Cites

No record.

References

No record.

Cite

APA: Copy

TAGHIPOUR, K., KHATIB, M.M., HEYHAT, M.R., VAEZI HIR, A.R., & SHABANIAN, E.. (2020). Structural controls on the hydrogeochemistry of Azarshahr travertine springs, NW Iran. IRANIAN JOURNAL OF GEOLOGY, 13(52 ), 105-122. SID. https://sid.ir/paper/129321/en

Vancouver: Copy

TAGHIPOUR K., KHATIB M.M., HEYHAT M.R., VAEZI HIR A.R., SHABANIAN E.. Structural controls on the hydrogeochemistry of Azarshahr travertine springs, NW Iran. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2020;13(52 ):105-122. Available from: https://sid.ir/paper/129321/en

IEEE: Copy

K. TAGHIPOUR, M.M. KHATIB, M.R. HEYHAT, A.R. VAEZI HIR, and E. SHABANIAN, “Structural controls on the hydrogeochemistry of Azarshahr travertine springs, NW Iran,” IRANIAN JOURNAL OF GEOLOGY, vol. 13, no. 52 , pp. 105–122, 2020, [Online]. Available: https://sid.ir/paper/129321/en

Related Journal Papers