Application of Cr-spinel mineral chemistry in petrogenetic evolution and tectonic setting of NE Kamyaran ophiolitic complex

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.

Veisinia a.; EBRAHIMI M.; MOKHTARI M.A.A.; AHMADIAN J.; AZIMZADEH A.M.

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:2018 | Volume:26 | Issue:3 Page(s): 581-596

Download Full-Text

Persian Verion

View:

288

Download:

Cites:

Information Journal Paper

Title

Application of Cr-spinel mineral chemistry in petrogenetic evolution and tectonic setting of NE Kamyaran ophiolitic complex

Author(s)

Keywords

Mineral chemistryQ1

Cr-spinelQ1

mantle peridotiteQ1

ophioliteQ2

KamyaranQ1

Abstract

Northeast Kamyaran ophiolitic complex is mainly composed of harzburgite along with small outcrops of lherzolite. Harzburgites are extensively altered to serpentinite. Small lenses of chromite mineralization are observed in harzburgites. The mineral assemblage present in the study harzburgite and lherzolite are olivine, orthopyroxene and clinopyroxene along with minor amount of spinel. Microprobe studies on the spinel indicate that it is Cr and Al bearing spinel (Cr-spinel) with very high Mg# (55. 2-71. 9) and Cr# (34. 3-45. 5) values and low values of TiO2 (with average value of 0. 6 wt%). Fe3+ content of the Cr-spinel in the study rocks is high (with average value of 0. 8 wt %) indicating that the crystallization occurred at high oxygen fugacity. According to the microprobe data, MgO content of olivine varies between 50. 04 and 52. 99 wt% and its composition is forsterite (Fo90. 68-91. 42). Based on the Mineral chemistry of spinel, peridotites of Northeast Kamyaran ophiolitic complex belong to residual depleted peridotites which have formed in mid ocean ridge tectonic setting.

Cites

No record.

References

No record.

Cite

APA: Copy

Veisinia, a., EBRAHIMI, M., MOKHTARI, M.A.A., AHMADIAN, J., & AZIMZADEH, A.M.. (2018). Application of Cr-spinel mineral chemistry in petrogenetic evolution and tectonic setting of NE Kamyaran ophiolitic complex. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 26(3 ), 581-596. SID. https://sid.ir/paper/405237/en

Vancouver: Copy

Veisinia a., EBRAHIMI M., MOKHTARI M.A.A., AHMADIAN J., AZIMZADEH A.M.. Application of Cr-spinel mineral chemistry in petrogenetic evolution and tectonic setting of NE Kamyaran ophiolitic complex. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2018;26(3 ):581-596. Available from: https://sid.ir/paper/405237/en

IEEE: Copy

a. Veisinia, M. EBRAHIMI, M.A.A. MOKHTARI, J. AHMADIAN, and A.M. AZIMZADEH, “Application of Cr-spinel mineral chemistry in petrogenetic evolution and tectonic setting of NE Kamyaran ophiolitic complex,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 26, no. 3 , pp. 581–596, 2018, [Online]. Available: https://sid.ir/paper/405237/en

Related Journal Papers

No record.

Related Seminar Papers

No record.

Related Plans

No record.

Recommended Workshops