Petrology, geochemistry and tectonomagmatic environment of southern volcanic rocks East of Mishu Mountains (west of Sefidkamar village - northwest of Iran)

Publish Year: 1400
نوع سند: مقاله کنفرانسی
زبان: English
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EISTC11_027

تاریخ نمایه سازی: 16 آذر 1400

Abstract:

The study area is located in the East of Azerbaijan, Northwest of Sefidkamar valley, and Northeast of Shabestar city. The igneous rocks of the region are volcanic type and the main minerals include Pyroxene, Amphibole, Olivin, and Plagioclase. The main textures in this rock flow, porphyry, and the sub-textures are glomeroporphyric, Trackytic, and sieve textures. According to Geochemical studies, these volcanic rocks have Basalt to Andesite basalt and Andesite compositions; These rocks are of the calk-alkaline basaltic type of the continental active margin environment. REE diagrams show enrichment of LREE than to HREE in the rocks which is showing they have originated from an enrichment mantle source. The primary magma of these rocks originated from the ۵-۱۰% partial melting rate of spinel-garnet Lherzolite mantle.

Authors

Fatemeh Gholampour Bami

Department of Geology, Faculty of Natural Sciences, University of Tabriz, Tabriz, Iran

Sayed Zia Hosseini

Department of Geology, Payame Noor University, Rafsanjan, Iran

Mohsen Moayyed

Department of Geology, Faculty of Natural Sciences, University of Tabriz, Tabriz, Iran