بررسی منطقه‌بندی پیوسته و ناپیوسته گارنت در میگماتیت‌های منطقه همدان و کاربردهای سنگ‌زایی آن

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه پیام نور

2 دانشگاه بوعلی سینا همدان

3 دانشگاه تبریز

چکیده

در منطقه همدان، سنگ­های میگماتیتی با ساختارهای مختلف رخنمون دارند که ساخت لایه­ای فراوانترین آنهاست. کانی­های شاخص متاپلیت­ها مانند گارنت (آلماندین)، استارولیت، آندالوزیت، سیلیمانیت، کیانیت، فیبرولیت، کردیریت، پلاژیوکلاز (آندزین) و اسپینل (هرسینیت) در میگماتیت­ها حضور دارند. گارنت در هر سه بخش روشن، تیره-روشن و تیره میگماتیت­ها حضور دارد و دستخوش رخدادهای مختلف دگرگونی (پیشرونده، پسرونده و ذوب بخشی) شده است. گارنت­ها دارای منطقه­بندی شیمیایی پیوسته و ناپیوسته برای عناصر شاخص Fe، Mg،  Mnو Ca هستند که الگوی رفتاری این عناصر در آنها یکسان نبوده و عواملی مثل وجود کانی­های تک­بلور چندهسته­ای، شرکت یا عدم شرکت گارنت­ها در فرایند ذوب­بخشی و چند دگرگونی منطقه در آن دخالت داشته­اند. ناپیوستگی در رشد بلورها بیانگر رشد مجدد طی یک رخداد دگرگونی مجزاست و می­تواند نشان دهنده دست کم دو رخداد دگرگونی باشد.

کلیدواژه‌ها

عنوان مقاله [English]

The study of continuous and discontinuous zoning of garnet mineral in the migmatites of the Hamedan region and its petrogenetic applications

نویسندگان [English]

  • Seyedeh Raziyeh Jafari 1
  • ali Asghar Sepahi 2
  • Mohsen Moazzen 3
  • Hosain Shahbazi 2
1
2
3
چکیده [English]

In the Hamedan region, migmatitic rocks with various structures cropped out that stromatic structure is the most abundant. Index minerals of metapelites such as garnet (almandine), staurolite, andalusite, sillimanite, kyanite, fibrolite, cordierite, plagioclase (andesine) and spinel (hercynite) are present in these rocks. Garnet has occurred in all three parts of leucosome, paleosome, and melanosome of migmatites and has been affected by various metamorphic events (progressive, retrograde, and partial melting). Garnets have continuous and discontinuous chemical zoning for index elements Fe, Mg, Mn and Ca, where the behavior of these elements is not the same. Some factors such as the presence of multi-nucleus single crystals, the participation or none participation of garnets in the process of partial melting and polymetamorphism of area have important role in it. The discontinuity in the growth of crystals represents a re-growth during an individual metamorphic event, and it can represent two metamorphic events.

کلیدواژه‌ها [English]

  • zoning
  • garnet
  • partial melting
  • migmatite
  • Hamedan

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  • تاریخ دریافت: 09 بهمن 1396
  • تاریخ بازنگری: 07 اردیبهشت 1397
  • تاریخ پذیرش: 12 خرداد 1397

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