Study of composition, source and tectonic setting of metapelite rocks from Mahneshan complex, NW, Iran
محل انتشار: دوفصلنامه زمین شناسی ژئوتکنیک، دوره: 4، شماره: 2
سال انتشار: 1387
نوع سند: مقاله ژورنالی
زبان: انگلیسی
مشاهده: 376
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شناسه ملی سند علمی:
JR_JGEO-4-2_006
تاریخ نمایه سازی: 30 آبان 1400
چکیده مقاله:
The Precambrian rocks of Mahneshan Complex in Northwestern Iran were affected by regional and contact metamorphism. At the Mahneshan Complex different types of igneous and metamorphic rocks are exposed. Metamorphic rocks including metapelites, amphibolites, metavolcanite, para-gneiss, metaperidotites and serpentinites. Metapelites are foliated at two directions. Exact petrographic and petrofabric studies on them show that three metamorphic phases including two regional and one contact are affected the rocks. Andalusite, staurolite, kyanite and garnet minerals are crystallized during second regional metamorphic phase. Geochemistry studies of metapelites shows that, Composition of old meta-sedimentary rocks (source of metapelites), are shale and greywacke. Discrimination diagrams indicate an arc related tectonic setting for the source of Mahneshan metapelites. Sources of Mahneshan metapelites are intermediate felsic igneous rocks (rhyolite or andesite) base on Geochemistry of immobile elements.
کلیدواژه ها:
نویسندگان
Adel Saki
Department of Geology, Faculty of Earth Science, Shahid Chamran University Ahvaz, Ahvaz, Iran
Gholamreza Mirzavand
Department of Geology, Faculty of Science, Islamic Azad University - Dezful Branch, Dezful, Iran