ضخامت پوسته و نقش آن در بارور بودن ماگما با استفاده از شیمی زیرکن: بررسی موردی مجموعه ماگمایی سنگان

نوع مقاله : مقاله پژوهشی

نویسندگان

1 گروه زمین شیمی، دانشکده علوم زمین، دانشگاه خوارزمی، ایران

2 گروه محیط زیست و تنوع زیستی، دانشکده زمین‌شناسی، دانشگاه سالزبورگ، اتریش

چکیده

فلات ایران در یکی از پیچیده­ترین موقعیت­های زمین پویایی کمربند آلپ-هیمالیا قرار دارد. منطقه معدنی سنگان بزرگترین منطقه سنگ آهن اسکارنی سنوزوئیک در دورترین بخش شرق کمان ماگمایی البرز در ایران است. توده‌های گرانیتوئیدی در منطقه معدنی سنگان شامل توده‌های بارور سرنوسر دربردارنده سینیت، سینوگرانیت و گرانیت و توده‌های عقیم سرخر و برمانی شامل مونزوگرانیت و سینوگرانیت هستند. در این پژوهش، از ترکیب 8 نمونه زیرکن از گرانیتوئید سرنوسر، سرخر و برمانی به عنوان یک ابزار اکتشافی مهم برای بازسازی دوباره تکامل ضخامت پوسته در کمان‌ ماگمایی سنگان استفاده شده است. ناهنجاری Eu/Eu* زیرکن (بهنجار شده با کندریت) با N(La/Yb) سنگ کل همبستگی مثبت دارد که از آن برای بازسازی ضخامت پوسته در زمان تشکیل توده­ها استفاده شده است. نتایج بررسی­های نشان می‌دهد که گرانیتوئیدهای بارور سرنوسر در پوسته ضخیم‌تری نسبت به گرانیتوئیدهای عقیم سرخر و برمانی تشکیل شده­اند.

کلیدواژه‌ها

عنوان مقاله [English]

Crustal thickness and its role in the magma fertility by using zircon chemistry: A case study of the Sangan magmatic complex

نویسندگان [English]

  • Majid Ghasemi Siani 1
  • Behzad Mehrabi 1
  • Franz Neubauer 2
1 Department of Geochemistry, Faculty of Earth Sciences, Kharazmi University, Iran
2 Department of Environment and Biodiversity, Geology Division, Paris-Lodron-University of Salzburg, A-5020 Salzburg, Austria
چکیده [English]

The Iranian plateau is located in one of the most complex geodynamic settings within the Alpine-Himalayan belt. The Sangan mining area is the largest Cenozoic skarn iron ore district in the far eastern part of the Alborz magmatic arc in Iran. Granitoid intrusions in the Sangan mining area are subdivided into the fertile Sarnowsar intrusion composed of syenite, syenogranite, and granite; and the barren Sarkhar and Bermani intrusions composed of monzogranite and syenogranite. In this study, we used the zircon geochemical composition from eight samples of Sarnowsar, Sarkhar and Bermani granitoids as an important exploration tool for reconstructing the crustal thickness and its evolution in the Sangan magmatic arc. Zircon Eu/Eu* [chondrite normalized] correlates with whole rock La/Yb, has been used to estimate the crustal thickness. Our results reveal that fertile Sarnowsar granitoids formed in the thicker crust than barren Sarkhar and Bermani granitoids.

کلیدواژه‌ها [English]

  • Crustal thickness
  • Magmatic fertility
  • Zircon chemistry
  • Eu anomaly
  • Sangan skarn

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  • تاریخ دریافت: 28 دی 1401
  • تاریخ بازنگری: 19 اسفند 1401
  • تاریخ پذیرش: 27 اسفند 1401

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