Granites and Earth Evolution.
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PETROLOGY AND GEOCHEMISTRY OF ALKALINE GRANITOID ROCKS FROM

THE MISHOW MOUNTAIN (NW IRAN)


Pirmohammadi F.*, Modjtahedy M.**, Gahangiry A.**, Amery A.**

*Geology Department, Faculty of science, Islamic Azad University/Shabestar Branch, Iran petrofarhad@yahoo.com

**Geology Department, Faculty of science, Tabriz University, Iran


Abstract

The intrusive body with an area of 10 kmē is located 20 km northwest of Shabestar, northwest Iran. This batholith is a part of west Alborz-Azarbaigaan zone that cuts Paleozoic rocks. The intrusive body consists of alkaline feldspar granite and granite in which the main mafic mineral is biotite. Furthermore, there is some enclave in these rocks. The study of the investigated samples shows that intrusive rocks north-west of Shabestar have two different generations. A part of the collected samples belongs to I-type granite and another one represents the A-type granite. It seems that this process is caused by contamination of alkaline magma with crustal materials, and primary magma of mantle is considered alkaline. Geochemistry of the rare earth elements shows that the tectonic setting of the body is compatible with Post Orogenic Granitoids (POG).

Key word: Shabestar, A-type granite, I-type granite, orogenic, biotite, alkaline.

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