دوره 29، شماره 4 - ( 10-1400 )                   جلد 29 شماره 4 صفحات 918-901 | برگشت به فهرست نسخه ها


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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
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

URL: http://ijcm.ir/article-1-1689-fa.html


1- دانشگاه لرستان
2- دانشگاه زنجان
3- دانشگاه بیرجند
4- موسسه زمین‌شناسی و ژئوفیزیک آکادمی علوم چین
چکیده:   (1415 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.     
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نوع مقاله: پژوهشي | موضوع مقاله: تخصصي

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