GEOTHERMOMETRY OF SKARNS IN THE NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE)

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.

TORABI GH.; NOURBEHESHT I.; SHIR DASHTZADEH N.; PIRNIA T.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2008 | Volume:15 | Issue:2 Page(s): 357-382

Download Full-Text

Persian Verion

View:

791

Download:

Cites:

Information Journal Paper

Title

GEOTHERMOMETRY OF SKARNS IN THE NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE)

Author(s)

TORABI GH. | NOURBEHESHT I. | SHIR DASHTZADEH N. | PIRNIA T. | Issue Writer Certificate

Keywords

GEATHERMOMETRYQ2

NAINQ2

OPHIOLITEQ2

SKARNQ2

TONALITEQ2

Abstract

One of the metamorphic rocks in the NAIN ophiolitic melange is SKARN which is formed during the contact metamorphism of intrusive TONALITEs with their neighboring limestone’s and carbonate parts of banded cherts. Minerals of these SKARNs consist of carbonate (calcite), clinopyroxene (diopside), garnet (grossular-andradite), wollastonite, sphene and epidote.Also TONALITEs contain quartz, plagioclase (albite), alkali feldspar (orthoclase), garnet (almandine-spessartine) and prehnite. Based on mineral assemblages of NAIN SKARNs as well as geothermometry of feldspars existing in relevant granites and also applications of different calibrations of garnet clinopyroxene geothermometer, the NAIN SKARNs form at temperatures of about 440 to 650°C at low pressure during a contact metamorphism which has occurred at hornblende hornfels to pyroxene hornfels facies.

Cites

No record.

References

STUDY OF SKARNS IN NORTH OF NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE, IRAN)

Cite

APA: Copy

TORABI, GH., NOURBEHESHT, I., SHIR DASHTZADEH, N., & PIRNIA, T.. (2008). GEOTHERMOMETRY OF SKARNS IN THE NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 15(2), 357-382. SID. https://sid.ir/paper/3990/en

Vancouver: Copy

TORABI GH., NOURBEHESHT I., SHIR DASHTZADEH N., PIRNIA T.. GEOTHERMOMETRY OF SKARNS IN THE NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2008;15(2):357-382. Available from: https://sid.ir/paper/3990/en

IEEE: Copy

GH. TORABI, I. NOURBEHESHT, N. SHIR DASHTZADEH, and T. PIRNIA, “GEOTHERMOMETRY OF SKARNS IN THE NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 15, no. 2, pp. 357–382, 2008, [Online]. Available: https://sid.ir/paper/3990/en

Related Journal Papers