کاربرد شیمی کانی در تعیین سنگ مادر و دمافشارسنجی سنگ‌های دگرگونی سرتیپ‌آباد (قروه-استان کردستان)

نوع مقاله : مقاله پژوهشی

نویسندگان

دانشگاه بوعلی سینا

چکیده

مجموعه دگرگونی سرتیپ­آباد در شهرستان قروه (کردستان)­ بخشی از پهنه  سنندج – سیرجان است. این مجموعه از سنگ­های دگرگونی ناحیه­ای شامل انواعی از شیست (آمفیبول­شیست، اکتینولیت­شیست، میکاشیست و گارنت شیست)، مرمر، متادیوریت، متاگابرو و پاراگنیس و نیز سنگ­های دگرگونی مجاورتی از نوع هورنفلس، تشکیل شده است. ترکیب کانی بیوتیت در شیست­ها و پاراگنیس از نوع سیدروفیلیت و در هورنفلس­ها و متادیوریت به ترتیب از نوع آنیتی و فلوگوپیتی است. آمفیبول­ها در پاراگنیس­ها از نوع هورنبلند و در متادیوریت­ها دارای ترکیب اکتینولیت هستند. گارنت­ها درگارنت میکاشیست از نوع آلماندن، پلاژیوکلازها در متادیوریت­ها و متاگابروها از نوع لابرادوریتی و در پاراگنیس­ها از نوع آندزین هستند. نتایج بررسی­های کانی­شناسی و دمافشارسنجی نشان می­دهد که طیف سنگ­های دگرگونی ناحیه­ای در گستره رخساره شیست سبز تا اپیدوت آمفیبولیت و در مرز بین پهنه­­های بیوتیت تا استارولیت تشکیل شده­اند در این راستا، برای انواع سنگ­های دگرگونی مجاورتی دست بالا رخساره آلبیت اپیدوت هورنفلس در نظر گرفته می­شود که برای سنگ­های دگرگونی مجاورتی بیانگر قلمرو رخساره آلبیت اپیدوت هورنفلس در پهنه ­های زوئیزیت تا آمفیبول است. در دماسنجی با روش­های تک کانی بیوتیت و با دماسنج تبادلی گارنت-بیوتیت، میانگین دما برای سنگ­های دگرگونی ناحیه­ای حدود ۵۶۷ درجه سانتی­گراد و برای سنگ­های دگرگونی مجاورتی حدود ۶۴۷ درجه سانتی­گراد به دست آمد. همچنین براساس دما-فشار سنجی به روش تک کانی بیوتیت، دما و فشار دگرگونی به طور میانگین برای مرحله دگرگونی M1 حدود ۵۷۸ درجه سانتی­گراد و ۱۶/۵ کیلوبار و برای مرحله M2 حدود ۵۶۵ درجه سانتی­گراد و ۶/۴ کیلوبار است. بر اساس بررسی­های صحرایی، شواهد سنگ­نگاری و داده­های زمین­شیمیایی سنگ­های مادر از سنگ­های رسوبی بوده و به ترتیب در سنگ­های پاراگنیسی، هورنفلس­ها و شیست­ها از نوع آرکوز، ماسه سنگ تیره و شیل هستند.       

کلیدواژه‌ها

عنوان مقاله [English]

Application of mineral chemistry in determination of protolith and thermobarometry of the Sartip Abad metamorphic rocks (Qorveh-Kurdistan Province)

نویسندگان [English]

  • Ashraf Torkian
  • Zahra Shirmohamadi
  • Fatemeh Kokabi
  • Mahsa Tahmasbi
Bu-Ali Sina University
چکیده [English]

The Sartip Abad metamorphic complex in Qorveh (Kurdistan Province) is located in the Sanandaj-Sirjan zone. The complex is composed of regional metamorphic rocks including contact metamorphic rocks (hornfels), variety of schists (amphibole schist, actinolite schist, mica schist, and garnet schist), marble, metadiorite, metagabbro, and paragneiss. In schists and paragneiss, biotite is siderophilite and in hornfels and metadiorite is anite to phlogopite in composition, respectively. Paragneiss and metadiorites include hornblende and actinolite. The garnets, in the garnet-mica schist, are almandine type, and plagioclase crystals in the metadiorites and metagabbros are labradorite type in composition, as well as their paragneiss have andesine- type plagioclase. Petrography and thermobarometric studies indicate that the different types of regional metamorphic rocks are formed in green schist to epidote-amphibolite facies and in the interval between biotite and staurolite zones. But for contact metamorphic rocks, the maximum facies is assumed albite-epidote hornfels in isograd of zoisite to amphibole. Thermometry calculations, using biotite single and garnet-biotite exchange, show that the average temperature for the metamorphic rocks of this region is about 567°C and for the contact metamorphic rocks is about 647 °C. Also, we used thermo-barometer methods for M1 and M2 metamorphic stages. Data are yielded, M1 stage temperature and pressure are about 578°C and 5.16 kb and for M2 stage ~565 °C and 4.6 kbar. Based on field relationships, petrographic evidence and geochemical data, protoliths are sedimentary rocks including greywackes/arkoses and shales for paragneiss, hornfels and schists, respectively.

کلیدواژه‌ها [English]

  • metamorphic
  • protolith
  • thermometer
  • metagabbro
  • paragneiss
  • Sanandaj – Sirjan

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مجله بلورشناسی و کانی شناسی ایران
دوره 31، شماره 1 - شماره پیاپی 89
فروردین 1402
صفحه 105-122

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  • تاریخ دریافت: 09 خرداد 1401
  • تاریخ بازنگری: 27 مرداد 1401
  • تاریخ پذیرش: 19 شهریور 1401

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