ذوب پریدوتیت بالای زون فرورانش عامل شرایط ریداکس ماگمایی توده‌های کانه‌دار ذخایر مس پورفیری ده‌سلم و چاه‌شلغمی؛ آنالیز درجا زیرکن

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه لرستان

2 دانشگاه زنجان

3 دانشگاه بیرجند

4 موسسه 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

عنوان مقاله [English]

Supra-subduction pridotite melting causing magmatic redox condition of Dehsalm and Chahshaljami Ore-bearing Cu porphyry deposits; In-situ Zircon Analysis

نویسندگان [English]

  • Almasi 1
  • Nabatian 2
  • Mahdavi 3
  • Li 4
1
2
3
4
چکیده [English]

 Oxygen fugacity (fO2) and zircon crystallization temperatures (Ti-in-zircon) of ore-bearing quartz monzonite intrusive rocks of ChahShaljami and Dehsalam Cu-Mo porphyry deposits were measured by using calculations of zircon trace element values and oxidation conditions of parental magma were investigated. The Ce4+/Ce3+ values for ChahShaljami and Dehsalam are in a range of 8 to 295 with an average of 125 and 3 to 171 with an average of 35, respectively, therefore they were not in the favorable range for porphyry mineralization. The estimated fO2 values for ChahShaljami and Dehsalam are in the range of ∆FMQ -1.8 to MFMQ +0.6 with an average of ∆FMQ -0.6 and ∆FMQ -1.3 to ∆FMQ -0.4 with an average of ∆FMQ -0.8 which is at least ∆FMQ +1 less than the values of porphyry copper mineralization in the world.. Based on the zircon log fO2 values of ore-bearing intrusive rock, the parental magma originated from partial melting of supra-subduction mantle peridotite zone within oceanic slab. Melting under unfavorable conditions (under magnetite-hematite (HM) buffer and in faylite-magnetite-quartz (FMQ) buffer condition, and lack of sufficient Cu and sulfur at the source), which is supported by evidences in deposit such as lack of magnetite-hematite intergrowths, was not ideal for porphyry Cu porphyry mineralization in the two regions. The results are supported also by previous whole-rock major and trace element geochemistry and Sr-Nd isotopic values.

کلیدواژه‌ها [English]

  • Zircon
  • oxygen fugacity
  • Cu porphyry
  • Chahshaljami
  • Dehsalm
  • peridotite

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  • تاریخ دریافت: 18 فروردین 1400
  • تاریخ بازنگری: 29 اردیبهشت 1400
  • تاریخ پذیرش: 17 خرداد 1400

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