PETROGRAPHY AND DEFORMATION OF ZARGOLI GRANITOID INTRUSION, NW OF ZAHEDAN, IRAN

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KANANIAN A.; KESHTGAR SHAHRIAR; ESMAEILI DARYOUSH

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Journal: JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT) Year:2006 | Volume:32 | Issue:3 (SECTION GEOLOGY 2) Page(s): 203-211

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Information Journal Paper

Title

PETROGRAPHY AND DEFORMATION OF ZARGOLI GRANITOID INTRUSION, NW OF ZAHEDAN, IRAN

Author(s)

KANANIAN A. | KESHTGAR SHAHRIAR | ESMAEILI DARYOUSH | Issue Writer Certificate

Keywords

ZAHEDANQ3

GRANITOIDQ3

MYLONITEQ3

SYN-TECTONICQ3

Abstract

The Zargoli intrusive body, which is located in the northern part of the ZAHEDAN-Saravan plutonic belt, is mostly composed of granodiorite, monzogranite and biotite granite. The GRANITOID rocks had deformed during dynamic metamorphism within numerous shear zones. Deformation intensity could be classified to low, medium and high grade based on the increasing stress from south towards the north. This deformation, which occurred under ductile to semi-ductile conditions, had formed the S-C MYLONITE in the granitic rocks. Occurrence of the cataclastic GRANITOID in the western margin of the pluton could be related to the final stage of deformation under brittle conditions. Brittle to ductile deformations of feldspars, along with oc-currence of the ribbon quartz, demonstrate that dynamic deformation occurred as medium to high grade greenshist facies between 300 to 450°C.Macroscopic and microscopic evidences show asyntectonic emplacement for the Zargoli intrusion.Seemingly, these intrusive rocks suffered dextral shear deformation in the early stage of crystallization or after solidification.

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APA: Copy

KANANIAN, A., KESHTGAR, SHAHRIAR, & ESMAEILI, DARYOUSH. (2006). PETROGRAPHY AND DEFORMATION OF ZARGOLI GRANITOID INTRUSION, NW OF ZAHEDAN, IRAN. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 32(3 (SECTION GEOLOGY 2)), 203-211. SID. https://sid.ir/paper/2293/en

Vancouver: Copy

KANANIAN A., KESHTGAR SHAHRIAR, ESMAEILI DARYOUSH. PETROGRAPHY AND DEFORMATION OF ZARGOLI GRANITOID INTRUSION, NW OF ZAHEDAN, IRAN. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2006;32(3 (SECTION GEOLOGY 2)):203-211. Available from: https://sid.ir/paper/2293/en

IEEE: Copy

A. KANANIAN, SHAHRIAR KESHTGAR, and DARYOUSH ESMAEILI, “PETROGRAPHY AND DEFORMATION OF ZARGOLI GRANITOID INTRUSION, NW OF ZAHEDAN, IRAN,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 32, no. 3 (SECTION GEOLOGY 2), pp. 203–211, 2006, [Online]. Available: https://sid.ir/paper/2293/en

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