شیمی‌کانی و زمین دماسنجی کلریت در منطقه زواری‌جان (شمال‌شرق بروجرد-ایران)

نوع مقاله : مقاله پژوهشی

نویسندگان

گروه زمین‌شناسی، دانشکده علوم پایه، واحد خرم‌آباد، دانشگاه آزاد اسلامی، خرم‌آباد، ایران

چکیده

در این مقاله، از روش زمین دماسنجی کلریت برای تعیین دمای دگرگونی درجه پائین و متوسط منطقه زواری‌جان واقع در شمال‌شرق بروجرد استفاده شده‌است. محاسبه فرمول ساختاری میانگین کلریت‌های انتخابی بر اساس 14 اکسیژن بیانگر تعداد کمتر از 91/2 اتم سیلیسیم در واحد فرمولی (apfu) و مجموع کاتیون‌های هشت‌‌وجهی نزدیک به 12apfu بوده که نشان‌دهنده کلریت هشت‌وجهی سه‌گانه است.کسرمولی در فاز بین لایه‌ای (Xc) نشان‌دهنده نبود اسمکتیت در فاز بین لایه‌ای و خلوص کلریت است. همه عناصر اصلی در کلریت با یکدیگر همخوانی دارند و تر کیب نمونه‌های کلریت از نوع رپیدولیت-پیکنوکلریت است. زمین دماسنجی کلریت نشان‌دهنده میانگین دمای 345 درجه سانتی‌گراد است که با میانگین دمای تشکیل کلریت برآمده از دگرسانی بیوتیت همخوانی دارد. این دما همچنین نشان‌دهنده تأثیر سیال­های گرمابی نوع متوسط دما یا کوهزایی در تشکیل کلریت است. براساس این نتایج، می‌توان گفت که شکل‌گیری کلریت در ناحیه مورد بررسی ناشی از عملکرد دگرگونی ناحیه‌ای بوده ‌است.     

کلیدواژه‌ها

عنوان مقاله [English]

Mineral chemistry and geothermometry of chlorite in Zavarijan area (NE Broujerd-Iran)

نویسندگان [English]

  • Kordi Sykan
  • Shahrokhiِ
Department of Geology, Faculty of Sciences, Khoramabad Branch, Islamic Azad University, Khoramabad, Iran
چکیده [English]

In this paper, the chlorite geothermometry method is used to estimate the low and medium temperature of metamorphism in Zavarijan area, northeast of Boroujerd. Structural formula recalculation for chlorite samples, based on 14 oxygen, show that Si cation numbers are less than 2.91(apfu), and the sum of octahedral cations is very close to 12(apfu), therefore both of them show an indication of trioctahedral chlorite. The mole fractions in interlayered phase(Xc) confirm the purity of chlorite and lack  of any smectite. All major elements in the chlorite are strongly corresponded with each other and chlorite samples composition are mainly ripidolite and pychnochlorite respectively. Chlorite geothermometry shows an average of 345ºC, so that corresponded with the average of temperature of chlorite crystallization that is resulted from biotite alteration. Also, this temperature indicates the mesothermal or orogenic fluids that have been importanat in generation of chlorite. Based on the present evidences, we can conclouded that formation of chlorite in the studied area is the result of regional metamorphism performance.

کلیدواژه‌ها [English]

  • chlorite
  • mole fractions
  • alteration
  • Smectite
  • Zavarijan
  • Broujerd

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  • تاریخ دریافت: 26 بهمن 1398
  • تاریخ بازنگری: 02 اردیبهشت 1399
  • تاریخ پذیرش: 03 خرداد 1399

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