شیمی کانی و شرایط تشکیل آمفیبولیت‌های مجموعه دگرگونی گیسور، شرق گناباد

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه لرستان

2 دانشگاه فردوسی مشهد

3 دانشگاه زنجان

چکیده

منطقه گیسور در شرق شهرستان گناباد قرار دارد و بخشی از شمال قطعه لوت محسوب می­شود. این منطقه شامل سنگ­های گرانیتوئیدی و مجموعه­ دگرگونی است. سنگ­های دگرگونی این منطقه به دو دسته رسی دگرگونه و آمفیبولیت­ها تقسیم می­شوند. براساس شواهد صحرایی و کانی­شناسی؛ سنگ­مادر آمفیبولیت­ها سنگ­ کربناتی ناخالص است. وجود گارنتِ پسازمین­ساخت و آمفیبول­های متقاطع و تصادفی در این آمفیبولیت­ها بیانگر عملکرد دگرگونی مجاورتی بر این سنگ­هاست. گارنت­ها رفتاری از آرمانی تا غیرآرمانی دارند. اعضای نهایی گارنت در این سنگ­ها متنوع و شامل Al-شورلومایت، اُوارُوایت، اسپسارتین، پیروپ، آلماندین، گروسولار، آندرادیت، موریموتایت و میجورایت هستند، اما الگوی نیم­رخ آن­ها مسطح است. آمفیبول از نوع فروهورنبلند تا فروچرماکیت و چرماکیت بوده و دارای منطقه­بندی ترکیبی است. بیوتیت کلریتی شده است. حضور کانی­های تیتانیت، اسفن و اپیدوت نشانه­ای از اثر گریزندگی اکسیژن است. بر پایه زمین دما فشارسنجی، مقدار دما و فشار برای آمفیبولیت­ها oC 609 - 534 و حدود kbar 4 - 2 به دست آمد. آمفیبولیت­های گیسور تا گستره رخساره آمفیبولیت میانی در هاله دگرگونی پیش رفته­اند. این سنگ­ها دستخوش یک دگرگونی برگشتی نیز شده­اند که دما و فشار آن oC489 و kbar 8/2 است و بیوتیت­های کلریتی شده دمایی کمتر از oC150 را نشان می­دهند.    

کلیدواژه‌ها

عنوان مقاله [English]

Mineral chemistry and petrogenesis of the Amphibolites of Geysour metamorphic complex, east of Gonabad

نویسندگان [English]

  • Pourmohammad 1
  • Ahmadi Khalaji 1
  • Homam 2
  • Ebrahimi 3
  • Esmaeili 3
  • Tahmasebi 1
1
2
3
چکیده [English]

The Geysour area is located east of Gonabad and is a part of the northern Lut block. The rocks in this area include granitoid and metamorphic rocks. Based on field and mineralogical evidence, the protolith of amphibolite rocks are calc-silicate. The metamorphic rocks of this region are divided into metapelites and amphibolites. Textures, such as post-tectonic garnet and random amphiboles, are indicative of contact metamorphism in amphibolites. Garnets behave from ideal to non-ideal. The end members of the garnet are varied in these rocks and include Al-schorlomite, uvarovite, spessartine, pyrope, almandine, grossular, andradite, morimotoite, and majorite, but their profile patterns are flat. The amphibole is of the ferrohornblende type to the ferrochermakite and chermakite, and has zoning. Biotite has converted to chlorite. The presence of titanite, hematite and epidote are an indication of the effect of oxygen fugacity. Temperature and pressure were calculated in the range of 534-609 oC and 2-<4 Kbar, respectively.  Geysour amphibolites have progressed to the mid-amphibolite facies in the metamorphic aureole. Also, these rocks were undergone a retrograde metamorphism where the temperature and pressure were 489oC and 2.8 kbar, respectively, and the chloritizied biotites exhibit temperatures below 150 oC.

کلیدواژه‌ها [English]

  • oxygen fugacity
  • garnet amphibolite
  • metamorphic aureole
  • Geysour
  • Gonabad
  • Lut block

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  • تاریخ دریافت: 08 آبان 1398
  • تاریخ بازنگری: 03 بهمن 1398
  • تاریخ پذیرش: 03 اسفند 1398

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