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Almasi, Nabatian, Mahdavi, Li. Supra-subduction pridotite melting causing magmatic redox condition of Dehsalm and Chahshaljami Ore-bearing Cu porphyry deposits; In-situ Zircon Analysis. www.ijcm.ir 2021; 29 (4) :901-918
URL: http://ijcm.ir/article-1-1689-fa.html
URL: http://ijcm.ir/article-1-1689-fa.html
الماسی علیرضا، نباتیان قاسم، مهدوی امیر، لی چیولی. ذوب پریدوتیت بالای زون فرورانش عامل شرایط ریداکس ماگمایی تودههای کانهدار ذخایر مس پورفیری دهسلم و چاه‌شلغمی؛ آنالیز درجا زیرکن. مجله بلورشناسی و کانی شناسی ایران. 1400; 29 (4) :901-918
علیرضا الماسی* 
1، قاسم نباتیان2 ، امیر مهدوی3 ، چیولی لی4
1، قاسم نباتیان2 ، امیر مهدوی3 ، چیولی لی4
1- دانشگاه لرستان
2- دانشگاه زنجان
3- دانشگاه بیرجند
4- موسسه زمین‌شناسی و ژئوفیزیک آکادمی علوم چین
2- دانشگاه زنجان
3- دانشگاه بیرجند
4- موسسه زمین‌شناسی و ژئوفیزیک آکادمی علوم چین
چکیده: (1338 مشاهده)
با استفاده از محاسبات مقادیر عنصر فرعی، فوگاسیته اکسیژن (fO2) و دمای تبلور زیرکنهای (Ti-in-zircon) تودههای نفوذی کوارتز مونزونیتی کانهدار کانسارهای مس-مولیبدن پورفیری چاه شلغمی و دهسلم محاسبه و شرایط اکسیداسیونی ماگمای مادر بررسی شد. مقادیر Ce4+/Ce3+ برای چاه شلغمی و دهسلم به ترتیب در بازههای 8 تا 295 با میانگین 125 و 3 تا 171 با میانگین 35 در بازه مطلوب برای کانیسازی پورفیری قرار نگرفت. مقادیر fO2 محاسبهشده برای چاه شلغمی در بازه 8/1- ∆FMQ تا 6/0+ ∆FMQ با میانگین 6/0- ∆FMQ و برای دهسلم در بازه محدود 3/1- ∆FMQ تا 4/0- ∆FMQ با میانگین 8/0- ∆FMQ قرار گرفت که حداقل به میزان 1+ ∆FMQ کمتر از مقادیر کانیسازی مس پورفیری شاخص در دنیا است. براساس مقادیر log fO2 زیرکن تودههای کانهدار، ماگمای مادر از ذوب بخشی پریدوتیت گوشتهای بالای زون فرورانش با دخالت ضعیف صفحه فرورانشی منشا گرفتهاست. ذوب در شرایط نامناسب (زیر خط بافر مگنتیت-هماتیت (HM) و در شرایط بافر فایالیت- مگنتیت-کوارتز (FMQ)، و نبود مقادیر مس و گوگرد کافی در منشا)، که با شواهد در درون ذخیره مانند نبود همرشدیهای مگنتیت-هماتیت حمایت میشود، برای
کانیسازی مس پورفیری در دو منطقه ایدهآل نبوده است. نتایج با دادههای ژئوشیمی عنصر اصلی و فرعی و مقادیر ایزوتوپی Sr-Nd سنگ کل قبلی نیز حمایت میشود.
کانیسازی مس پورفیری در دو منطقه ایدهآل نبوده است. نتایج با دادههای ژئوشیمی عنصر اصلی و فرعی و مقادیر ایزوتوپی Sr-Nd سنگ کل قبلی نیز حمایت میشود.
واژه‌های کلیدی: زیرکن، فوگاسیته اکسیژن، مس پورفیری، چاه شلغمی، دهسلم، پریدوتیت.
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