Microstructure analysis on estimation of deformation conditions in the Bibi Maryam granitoid, northern Sistan suture zone, East of 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.

etemadkhah z.; KHATIB M.M.; ZARRINKOUB M.H.

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

Journal Paper

Paper Information

Journal: Researches in Earth Sciences Year:2018 | Volume:9 | Issue:34 Page(s): 15-28

Download Full-Text

Persian Verion

View:

414

Download:

Cites:

Information Journal Paper

Title

Microstructure analysis on estimation of deformation conditions in the Bibi Maryam granitoid, northern Sistan suture zone, East of Iran

Author(s)

etemadkhah z. | KHATIB M.M. | ZARRINKOUB M.H. | Issue Writer Certificate

Keywords

Sistan suture zoneQ1

Preferred orientationQ1

MicrostructureQ2

GranitoidQ2

NehbandanQ2

Abstract

The Bibi Maryam Granitoid with NW– SE general trend has intruded into Nehbandan ophiolite complex in the northern Sistan suture zone. The massif was influenced by syntectonic emplacement and cooling and thus has recorded short-lived geological events related to crustal deformation. Development of microfabrics in this Granitoid from magmatic to low temperature solid-state reflect the microstructural evolution with decreasing melt content during crystallization. There are clear evidences of synmagmatic deformation fabrics as well as evidences of high-T solid-state deformation that suggest these fabrics have been developed during or just after complete crystallization of magma. With continuous deformation, the low-temperature fabrics characterized by subgrains rotation recrystallization in quartz, orientation of quartz fine-grains and microfaults in feldspar. The foliation trajectories through out the massif show a dominant NW– SE orientation. The presence of synmagmatic deformation Microstructures and the concordance of solid-state mesoscopic-scale planar fabrics with general regional structures imply that the time relationship between fabric development in the Granitoid and regional tectonics within this part of Sistan zone.

Cites

No record.

References

No record.

Cite

APA: Copy

etemadkhah, z., KHATIB, M.M., & ZARRINKOUB, M.H.. (2018). Microstructure analysis on estimation of deformation conditions in the Bibi Maryam granitoid, northern Sistan suture zone, East of Iran. RESEARCHES IN EARTH SCIENCES, 9(34 ), 15-28. SID. https://sid.ir/paper/207410/en

Vancouver: Copy

etemadkhah z., KHATIB M.M., ZARRINKOUB M.H.. Microstructure analysis on estimation of deformation conditions in the Bibi Maryam granitoid, northern Sistan suture zone, East of Iran. RESEARCHES IN EARTH SCIENCES[Internet]. 2018;9(34 ):15-28. Available from: https://sid.ir/paper/207410/en

IEEE: Copy

z. etemadkhah, M.M. KHATIB, and M.H. ZARRINKOUB, “Microstructure analysis on estimation of deformation conditions in the Bibi Maryam granitoid, northern Sistan suture zone, East of Iran,” RESEARCHES IN EARTH SCIENCES, vol. 9, no. 34 , pp. 15–28, 2018, [Online]. Available: https://sid.ir/paper/207410/en

Related Journal Papers