سامانه مدیریت نشریات علمی دانشگاه دامغان

حسن زاده, تهمینه, حیدری, سید مهران, قلمقاش, جلیل, محبی, آیدا. (1404). بررسی ماگما و کنترل‌کننده‌های کانه‌زایی طلا (مس) فراگرمایی زواریان (سلفچگان) در مقایسه با طلای فراگرمایی ساری‌گونای (قروه). مجله زمین شیمی ایران, 29(4), 759-778. doi: 10.52547/ijcm.29.4.759
تهمینه حسن زاده; سید مهران حیدری; جلیل قلمقاش; آیدا محبی. "بررسی ماگما و کنترل‌کننده‌های کانه‌زایی طلا (مس) فراگرمایی زواریان (سلفچگان) در مقایسه با طلای فراگرمایی ساری‌گونای (قروه)". مجله زمین شیمی ایران, 29, 4, 1404, 759-778. doi: 10.52547/ijcm.29.4.759
حسن زاده, تهمینه, حیدری, سید مهران, قلمقاش, جلیل, محبی, آیدا. (1404). 'بررسی ماگما و کنترل‌کننده‌های کانه‌زایی طلا (مس) فراگرمایی زواریان (سلفچگان) در مقایسه با طلای فراگرمایی ساری‌گونای (قروه)', مجله زمین شیمی ایران, 29(4), pp. 759-778. doi: 10.52547/ijcm.29.4.759
حسن زاده, تهمینه, حیدری, سید مهران, قلمقاش, جلیل, محبی, آیدا. بررسی ماگما و کنترل‌کننده‌های کانه‌زایی طلا (مس) فراگرمایی زواریان (سلفچگان) در مقایسه با طلای فراگرمایی ساری‌گونای (قروه). مجله زمین شیمی ایران, 1404; 29(4): 759-778. doi: 10.52547/ijcm.29.4.759

بررسی ماگما و کنترل‌کننده‌های کانه‌زایی طلا (مس) فراگرمایی زواریان (سلفچگان) در مقایسه با طلای فراگرمایی ساری‌گونای (قروه)

مجله بلورشناسی و کانی شناسی ایران
مقاله 4، دوره 29، شماره 4 - شماره پیاپی 84، دی 1400، صفحه 759-778    اصل مقاله (7.84 M)
شناسه دیجیتال (DOI): 10.52547/ijcm.29.4.759
نویسندگان
تهمینه حسن زاده؛ سید مهران حیدری* ؛ جلیل قلمقاش؛ آیدا محبی
سازمان زمین شناسی و معدنی کشور
چکیده
کانسار طلا (مس) زواریان در میانه کمان ماگمایی ارومیه-دختر، در مخروطی آتشفشانی با واحدهای آندزی-بازالت، آندزیتی و توده­های گرانودیوریتی واقع است. این مجموعه دارای ماهیت آهکی قلیایی و الگوی تغییرات عناصر کمیاب و خاکی نادر (غنی­شدگی عناصر سنگ دوست بزرگ یون، عناصر خاکی نادر سبک نسبت ­به عناصر با شدت میدان بالا، عناصر خاکی نادر سنگین، ناهنجاری منفی  Ti,Nbو مقادیر پایین Nb/Y) ماگماهای وابسته به کمان است. بررسی­های ساختاری به­نقش کلیدی پهنه­های برشی راستگرد به­عنوان کنترل­کننده حوضه­های رسوبی و ایجاد شرایط لازم برای کشش­های محلی و خروج ماگما اشاره دارد. پراکندگی و نوع دگرسانی­های گرمابی، رگه­های کانه­دار درون نفوذی­ها­ و حضور مگنتیت، تورمالین و کالکوپیریت ­نقش سیال­های ماگمایی رادر تشکیل کانه­زایی نشان می­دهند. این سیال­ها دارای دمای همگن­شدگی 220 تا oC 350 و شوری 15-10% وزنی نمک طعام هستند. براساس مقایسه این کانه­زایی با کانسار ساری­گونای در شمال­ غرب پهنه سنندج-سیرجان، فازهای ماگمایی میوسن مربوط به تشکیل پهنه­های برشی و ایجاد کشش­های محلی در فازهای کوهزایی پس از برخوردی هستند که با افزایش نقش سیال­های جوی و آمیختگی آنها با سیال­های ماگمایی همراه است.       
کلیدواژه‌ها
طلای فراگرمایی؛ زواریان؛ سلفچگان؛ ساری‌گونای؛ کوهین؛ ایران
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