سامانه مدیریت نشریات علمی دانشگاه دامغان

الماسی, علیرضا, نباتیان, قاسم, مهدوی, امیر, لی, چیولی. (1404). ذوب پریدوتیت بالای زون فرورانش عامل شرایط ریداکس ماگمایی توده‌های کانه‌دار ذخایر مس پورفیری ده‌سلم و چاه‌شلغمی؛ آنالیز درجا زیرکن. مجله زمین شیمی ایران, 29(4), 901-918. doi: 10.52547/ijcm.29.4.901
علیرضا الماسی; قاسم نباتیان; امیر مهدوی; چیولی لی. "ذوب پریدوتیت بالای زون فرورانش عامل شرایط ریداکس ماگمایی توده‌های کانه‌دار ذخایر مس پورفیری ده‌سلم و چاه‌شلغمی؛ آنالیز درجا زیرکن". مجله زمین شیمی ایران, 29, 4, 1404, 901-918. doi: 10.52547/ijcm.29.4.901
الماسی, علیرضا, نباتیان, قاسم, مهدوی, امیر, لی, چیولی. (1404). 'ذوب پریدوتیت بالای زون فرورانش عامل شرایط ریداکس ماگمایی توده‌های کانه‌دار ذخایر مس پورفیری ده‌سلم و چاه‌شلغمی؛ آنالیز درجا زیرکن', مجله زمین شیمی ایران, 29(4), pp. 901-918. doi: 10.52547/ijcm.29.4.901
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 زمین شیمی ایران, 1404; 29(4): 901-918. doi: 10.52547/ijcm.29.4.901

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
مقاله 14، دوره 29، شماره 4 - شماره پیاپی 84، دی 1400، صفحه 901-918    اصل مقاله (2.14 M)
شناسه دیجیتال (DOI): 10.52547/ijcm.29.4.901
نویسندگان
علیرضا الماسی* 1؛ قاسم نباتیان2؛ امیر مهدوی3؛ چیولی لی4
1دانشگاه لرستان
2دانشگاه زنجان
3دانشگاه بیرجند
4موسسه زمین‌شناسی و ژئوفیزیک آکادمی علوم چین
چکیده
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.     
کلیدواژه‌ها
زیرکن؛ فوگاسیته اکسیژن؛ مس پورفیری؛ چاه شلغمی؛ ده‌سلم؛ پریدوتیت
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