کاربرد شیمی‌کانی‌ها در تعیین شرایط تشکیل گرانیت‌ اسماعیل آباد در منطقه پشت بادام (خرد قاره شرق- ایران مرکزی)

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه پیام نور

2 دانشگاه اصفهان

چکیده

توده گرانیتی اسماعیل آباد با سن تریاس پسین در بخش مرکزی پهنه پشت بادام(خرد قاره شرق- ایران مرکزی)، در شمال شرقی استان یزد قرار دارد. این توده گرانیتی به درون سنگ‌های دگرگونی مجموعه پشت بادام نفوذ کرده و به وسیله رسوبات آهکی کرتاسه پوشانده شده است. مجموعه کانی‌های سازنده گرانیت‌های مورد بررسی شامل کوارتز، فلدسپار پتاسیم (ارتوکلاز)، پلاژیوکلاز (آندزین و الیگوکلاز)، آمفیبول (مگنزیوهورنبلند)، بیوتیت (غنی از منیزیم)، آپاتیت، تیتانیت و زیرکن است. بر پایه نتایج شیمی‌کانی‌ها، آمفیبول‌های موجود در گرانیت‌های مورد بررسی دارای ماهیت آذرین هستند. بیوتیت‌های موجود در این سنگ‌ها شامل بیوتیت‌های غنی از منیزیم بوده که مشخصات شیمی‌کانی آن‌ها نشان‌دهنده ترکیب بیوتیت‌های اولیه‌ی برآمده از تبلور یک ماگمای آهکی-قلیایی است. ترکیب شیمیایی آمفیبول‌ها و بیوتیت‌های موجود در گرانیت‌های اسماعیل آباد نشان دهنده وابستگی آن‌ها به گرانیت‌های نوع  I است و در محیطی با گریزندگی بالای اکسیژن تشکیل شده‌اند. محاسبات زمین دما-فشارسنجی، دمای بین 550 تا 700 درجه سانتی‌گراد و گستره‌ی فشار 2 تا 8/3 کیلوبار را نشان می‌دهد. با توجه به جایگاه وسن سنگ‌های مورد بررسی، تشکیل این توده‌ی گرانیتی را می‌توان مربوط به بسته‌شدن و فرورانش اقیانوس پالئوتتیس در بخش غربی خردقاره شرق- ایران مرکزی در نظر گرفت که ادامه روند برخورد قاره‌ای باعث شروع فعالیت‌های آذرین نفوذی ایجاد این توده‌ی گرانیتی در منطقه شده­است.     

کلیدواژه‌ها

عنوان مقاله [English]

Mineral chemistry using for evaluation of the Esmaeilabad granite generation in the Posht-e-Badam area (Central- East Iranian Microcontinent)

نویسندگان [English]

  • khadijeh Khalili 1
  • Narges Nosouhian 2
  • Ghodrat Torabi 2
1
2
چکیده [English]

The Esmaeilabad granitic body with the Late Triassic age is situated in the central part of the Posht-e-Badam block (Central- East Iranian Microcontinent), in the northeastern of the Yazd Province. This granitic body cross cut the metamorphic rocks of the Posht-e-Badam complex and covered by the Cretaceous limestone. Rock forming minerals of the studied granites are K-feldspar (orthoclase), plagioclase (andesine, oligoclase), quartz, amphibole (magnesio-hornblende), biotite, apatite, titanite and zircon. According to the mineral chemistry analyses, amphiboles represent the igneous nature. Biotites are rich in Magnesium. Chemical characteristics of biotites indicate that they are primary biotites which are generated by calc-alkaline magma. Chemical composition of the amphiboles and biotites in the Esmaeilabad granites suggest that they belong to the I-type granites and generate in an environment with high fO2. Geothermobarometry estimations yield temperatures between 550 to 700 oC and pressures in the range of 2 to 3.8 kbar. Based on the geological position and age of the studied rocks, generation of this granitic body can be related to the subduction and closure of the Paleo-Tethys Ocean in the western part of the Central- East Iranian Microcontinent, which can be the reason for granitic plutonism in this area.

کلیدواژه‌ها [English]

  • Mineral chemistry
  • geothermobarometry
  • granite
  • Esmaeilabad
  • Posht-e-Badam
  • Paleo-Tethys
  • Central- East Iranian Microcontinent

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  • تاریخ دریافت: 08 اردیبهشت 1397
  • تاریخ بازنگری: 17 مرداد 1397
  • تاریخ پذیرش: 12 شهریور 1397

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