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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
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
گروه مهندسی معدن مرکز آموزش عالی شهید باکری میاندوآب-دانشگاه ارومیه، 5978159، میاندوآب، ایران
چکیده: (1087 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.
واژه‌های کلیدی: سنگهای آپینیت، گرانیت، سنگ‌زایی، زمین‌شیمی، پهنه سنندج سیرجان، نقده، شمال غرب ایران.
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