زئولیت‌های پُر‌کننده‌ی حفره‌ها و بادامک‌ها در سنگ‌های آتشفشانی شمال‌غرب کوه دوازده امام، شمال ایران‌مرکزی

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه خوارزمی

2 دانشگاه تهران

چکیده

بخش شمال­غربی مجموعه­ی آتشفشانی- رسوبی کوه دوازده امام، در شمال ایران مرکزی و در 135 کیلومتری جنوب شرق تهران واقع است. گدازه­ها و دایک­های حدّواسط­- بازی و بیشتر بازی ائوسن و الیگوسن این مجموعه در اثر سیّال­های ­گرمابی، احتمالاً همراه با مشارکت آب­های جوّی دستخوش درجات مختلفی از دگرسانی شده­اند. این دگرسانی­ها در دو مرحله سبب تشکیل زئولیت و دیگر کانی­های ثانویه گردیده است. فعّالیّت سیّال گرمابی در مرحله­ی نخست، سبب ته­نشینی فیلوسیلیکات­های مافیک (سلادونیت، لایه­های ترکیبی سلادونیت- نانترونیت، اسمکتیت)، کلسیت و زئولیت­های سدیمی (آنالسیم، تتراناترولیت، ناترولیت و شابازیت­- Ca) شده است؛ در مرحله­ی دوّم، فعّالیّت سیّال­های گرمابی احتمالاً همراه با مشارکت آب جوّی شرایط را جهت شکل­گیری زئولیت­های کلسیمی-­ سدیمی و در نتیجه نهشته شدن استیلبیت­- Ca، مزولیت و تامسونیت فراهم کرده است. تغییر در دما، pH، مقادیر CO2 و H2O، نسبت Si/Al و نوع سنگ بستر، عواملی هستند که سبب تنوّع کانی­زایی طیّ این دو مرحله شده­اند. بالاترین و پایین­ترین دمای زئولیت­زایی مرحله­ی نخست را می­توان حدود °C 145 برای آنالسیم و °C 90 برای شابازیت­- Ca و برای مرحله­ی دوّم، حدود  °C75 برای استیلبیت­- Ca و °C 65 برای تامسونیت در نظر گرفت.     

کلیدواژه‌ها

عنوان مقاله [English]

Zeolites filling cavities and amigdales of basic volcanic rocks in NW of Davazdah-Emam mountain, north Central Iran

نویسندگان [English]

  • sahar Koohfar 1
  • Amirali Tabbakh Shabani 1
  • kamalodin Bazargani-Guilani 2
  • Morteza Delavari Kooshan 1
1 Kharazmi University
2 Tehran University
چکیده [English]

The north western part of volcano-sedimentary complex of Davazdah-Emam mountain in north of Central Iran is located about 135 km SE Tehran. The Eocene to Oligocene volcanic rocks and dikes of intermediate to mainly basic of complex under the influence of hydrothermal fluids, probably associated with the involvement of meteoric water, experienced different degrees of alteration. The alteration occurred in two steps forming mafic phyllosilicates (celadonite, mixed layers of celadonite-nontronite, smectite), calcite and sodic zeolites (analcime, tetranatrolite, natrolite and chabazite-Ca) at the first step and in the second step, hydrothermal associated possibly with the involvement of the meteoric water facilitated the disposition of calcic-sodic zeolites such as stilbite-Ca, mesolite and thomsonite. Variatians in temperatures, pH, CO2 and H2O values, Si/Al ratio and host rocks types are the parameters that causes the diversities of mineralization through out the two steps. Maximum and minimum temperatures of zeolite formation for the first stage can be estimated around 145°C for analcime and 90°C for chabazite-Ca and for second stage, around 75°C for stilbite-Ca and 65°C for thomsonite.

کلیدواژه‌ها [English]

  • zeolite
  • hydrothermal alteration
  • secondary minerals
  • Davazdah-Emam mountain

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  • تاریخ دریافت: 24 تیر 1396
  • تاریخ بازنگری: 08 آبان 1396
  • تاریخ پذیرش: 27 آذر 1396

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