MINERALOGY OF AMPHIBOLITES AND EPIDOTE AMPHIBOLITES FROM SOUTH OF SALMAS, NW OF IRAN; DETERMINATION THERMODYNAMIC CONDITIONS OF EPIDOTE AMPHIBOLITE TO AMPHIBOLITE SUB-FACIES TRANSFORMATION

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.

AHANGARI M.; MOAZZEN M.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Geology Year:2011 | Volume:5 | Issue:19 Page(s): 93-106

Download Full-Text

Persian Verion

View:

2,347

Download:

Cites:

Information Journal Paper

Title

MINERALOGY OF AMPHIBOLITES AND EPIDOTE AMPHIBOLITES FROM SOUTH OF SALMAS, NW OF IRAN; DETERMINATION THERMODYNAMIC CONDITIONS OF EPIDOTE AMPHIBOLITE TO AMPHIBOLITE SUB-FACIES TRANSFORMATION

Author(s)

AHANGARI M. | MOAZZEN M. | Issue Writer Certificate

Keywords

AMPHIBOLITEQ2

EPIDOTE- AMPHIBOLITEQ2

GEOTHERMOBAROMETERYQ2

MINERAL CHEMISTRYQ1

SALMASQ2

Abstract

AMPHIBOLITEs and epidote AMPHIBOLITEs are the main exposures of metabasites in south of SALMAS area. MINERAL CHEMISTRY of these two rock groups is different, and shows differences in the P-T conditions during prograde metamorphism. Study of amphibole chemistry show increases of tschermakite and crossite end members in amphiboles from epidote AMPHIBOLITEs toward amphiboles within the AMPHIBOLITE samples, while increasing of the edenite content during transformation from epidote AMPHIBOLITE to AMPHIBOLITE is negligible. On the basis of MINERAL CHEMISTRY, rising of temperature was more effective than rising of pressure in transformation of epidote AMPHIBOLITEs to AMPHIBOLITEs in the studied samples. According to geothermobarometeric studies, epidote AMPHIBOLITEs and AMPHIBOLITEs were metamorphosed at 500±20oC, 2-5 (commonly less than 5) Kbar and 600±20oC, 6-8 Kbar conditions, respectively.

Cites

No record.

References

No record.

Cite

APA: Copy

AHANGARI, M., & MOAZZEN, M.. (2011). MINERALOGY OF AMPHIBOLITES AND EPIDOTE AMPHIBOLITES FROM SOUTH OF SALMAS, NW OF IRAN; DETERMINATION THERMODYNAMIC CONDITIONS OF EPIDOTE AMPHIBOLITE TO AMPHIBOLITE SUB-FACIES TRANSFORMATION. IRANIAN JOURNAL OF GEOLOGY, 5(19), 93-106. SID. https://sid.ir/paper/129433/en

Vancouver: Copy

AHANGARI M., MOAZZEN M.. MINERALOGY OF AMPHIBOLITES AND EPIDOTE AMPHIBOLITES FROM SOUTH OF SALMAS, NW OF IRAN; DETERMINATION THERMODYNAMIC CONDITIONS OF EPIDOTE AMPHIBOLITE TO AMPHIBOLITE SUB-FACIES TRANSFORMATION. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2011;5(19):93-106. Available from: https://sid.ir/paper/129433/en

IEEE: Copy

M. AHANGARI, and M. MOAZZEN, “MINERALOGY OF AMPHIBOLITES AND EPIDOTE AMPHIBOLITES FROM SOUTH OF SALMAS, NW OF IRAN; DETERMINATION THERMODYNAMIC CONDITIONS OF EPIDOTE AMPHIBOLITE TO AMPHIBOLITE SUB-FACIES TRANSFORMATION,” IRANIAN JOURNAL OF GEOLOGY, vol. 5, no. 19, pp. 93–106, 2011, [Online]. Available: https://sid.ir/paper/129433/en

Related Journal Papers