زمین‌شیمی و سنگ‌زایی سنگ‌های آپینیتی و سنگ‌های گرانیتی همراه آن‌ در جنوب غرب نقده- شمال غرب ایران

نوع مقاله : مقاله پژوهشی

نویسنده

گروه مهندسی معدن مرکز آموزش عالی شهید باکری میاندوآب-دانشگاه ارومیه، 5978159، میاندوآب، ایران

چکیده

توده­های نفوذی در جنوب غرب نقده در پهنه سنندج- سیرجان در شمال غرب ایران رخنمون یافته­اند. بخشی از این توده­ها، سنگ­های آپینیتی مافیک- حدواسط نزدیک آهکی قلیایی هستند. سنگ­های گرانیت همراه آن، با ماگمای آهکی قلیایی غنی از پتاسیم و به شدت دگرگون یافته هستند. بررسی­های زمین­شیمیایی سنگ­های آپینیتی و گرانیتی همراه آن غنی­شدگی از عناصر خاکی نادر سبک (LREE) نسبت به عناصر خاکی نادر سنگین (HREE)، غنی شدگی عناصر سنگ دوست بزرگ یون (LILE) و ناهنجاری منفی عناصر Nb Ta, را نشان می­دهند. بررسی­های زمین­ساختی سنگ­های آپینیتی و گرانیتی همراه آن محیط قوس قاره­ای را نشان داده و خاستگاه آپینیت را گوشته سنگ کره­ای با اثر سیال­های فرورانشی و خاستگاه گرانیت­ها را آمیزه گوشته سست کره­ای- سنگ کره­ای با دخالت پوسته ماسه سنگ تیره نشان می­دهند. به احتمال بسیار، سنگ­های آپینیتی در محل قوس قاره­ای همراه با عقبگرد پوسته فرورونده و اثر سیال­های فرورانشی در شرایط غنی از آب تبلور یافته­اند. سنگ­های گرانیتی در اثر شکست سنگ کره فرورانشی نئوتتیس و ایجاد پنجره فرورانشی و بالا رانده شدن سست کره، از ذوب آمیزه گوشته سست کره ای-سنگ کره­ای و رسوب­های ماسه سنگ تیره پوسته قاره­ای شکل گرفته­اند. ماگما دچار جدایش بلوری و تبلور طولانی مدتی در بخش عمقی مخزن ماگمایی شده که در پایان توانسته است ماگمای گرانیتی به شدت دگرگون شده­ای­ را در عمق کم پوسته­ای در محل شکستگی­ها جایگیری کند.    

کلیدواژه‌ها


عنوان مقاله [English]

Geochemistry and petrogenesis of appinite rocks and accompanied granite rocks from SW Naghadeh-NW Iran

نویسنده [English]

  • Maryam Yazdani
Shahid Bakeri Higher Education Centre of Miandoab, Urmia University
چکیده [English]

Intrusive rocks are exposed in southwest of Naqdeh in the Sanandaj-Sirjan zone, northwest Iran. There are mafic-intermediate appinitic rocks with calc-alkaline affinity. The accompanying granite is strongly evolved with the affinity of calc-alkaline and rich in potassium. The geochemical analysis of appinite and granitic rocks display LREE enrichment relative to HREE, enrichment of LILE elements, and negative Th and Nb anomalies. According to discrimination diagrams, appinite and granite rocks formed in the continental arc tectonic setting. The appinitic rocks have a lithospheric mantle with subducting slab fluids source. The granitic rocks have an asthenospheric-lithospheric mantle with metagreywaky continental crust contamination. We suggest that appinitic magma formed by roll-back of subducted Neo-Tethys oceanic lithosphere and granitic magma formed by breck-off the subducted Neo-Tethyan oceanic slab. The asthenospheric upwelling would also have provided enough heat for the partial melting of continental crust. It is possible that magma formed at a great depth and underwent a long period of fractional crystallization. Finally, evolved granitic rocks have been placed at a shallow depth of the crust.

کلیدواژه‌ها [English]

  • Appinite rocks
  • granite
  • petrogenesis
  • gechemistry
  • Sanandaj-Sirjan Zone
  • Naghadeh
  • NW Iran
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