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Yazdani M. Geochemistry and petrogenesis of appinite rocks and accompanied granite rocks from SW Naghadeh-NW Iran. www.ijcm.ir 2023; 31 (4) :633-648
URL: http://ijcm.ir/article-1-1795-fa.html
یزدانی مریم. زمین‌شیمی و سنگ‌زایی سنگ‌های آپینیتی و سنگ‌های گرانیتی همراه آن‌ در جنوب غرب نقده- شمال غرب ایران. مجله بلورشناسی و کانی شناسی ایران. 1402; 31 (4) :633-648

URL: http://ijcm.ir/article-1-1795-fa.html


گروه مهندسی معدن مرکز آموزش عالی شهید باکری میاندوآب-دانشگاه ارومیه، 5978159، میاندوآب، ایران
چکیده:   (988 مشاهده)
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.    
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نوع مقاله: پژوهشي | موضوع مقاله: تخصصي

فهرست منابع
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