دوره 27، شماره 1 - ( 1-1398 )
جلد 27 شماره 1 صفحات 220-207 |
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Nakhaei M, Mohammadi S S, Rasa I, Samiee S. Study of mineralogy, geochemistry and elemental behavior in the process of bentonites formation in Sarbisheh area (South Khorasan, east of Iran). www.ijcm.ir 2019; 27 (1) :207-220
URL: http://ijcm.ir/article-1-1236-fa.html
URL: http://ijcm.ir/article-1-1236-fa.html
نخعی ملیحه، محمدی سید سعید، رسا ایرج، سمیعی سمیه. بررسی کانیشناسی، زمین‌شیمی و رفتار عناصر در فرایند تشکیل بنتونیتهای منطقه سربیشه (خراسان جنوبی، شرق ایران). مجله بلورشناسی و کانی شناسی ایران. 1398; 27 (1) :207-220
ملیحه نخعی* 
1، سید سعید محمدی2 ، ایرج رسا3 ، سمیه سمیعی1
1، سید سعید محمدی2 ، ایرج رسا3 ، سمیه سمیعی1
1- دانشگاه صنعتی بیرجند
2- دانشگاه بیرجند
3- دانشگاه شهید بهشتی
2- دانشگاه بیرجند
3- دانشگاه شهید بهشتی
چکیده: (3215 مشاهده)
فعالیتهای آتشفشانی اسیدی تا حدواسط ترشیری و عملکرد پهنههای گسلی در منطقه سربیشه، شرایط مناسبی را برای تشکیل بنتونیت به ویژه در نهشتههای آذرآواری فراهم نموده است. پهنههای بنتونیتی جنوبشرق گندکان، کلاته پدران، گلاب، گلستان، آسفیچ، حسن کلنگی و کنگان در گستره نقشه زمینشناسی 1:100000 سربیشه هدف این پژوهش بودهاند. پردازش تصاویر ماهوارهای بیانگر رخداد دگرسانی گسترده رسی باحضور کانی مونتموریلونیت است. برداشتهای صحرایی و بررسیهای کانیشناسی به روش پراش پرتوی X (XRD)، پردازشهای ماهوارهای و تشکیل بنتونیت در این مناطق را تایید نمود. کانیهای اصلی تشکیل دهنده این بنتونیتها شامل مونتموریلونیت، آنورتیت وکریستوبالیت هستند. بر اساس دادههای موجود، بنتونیت حسن کلنگی از نوع سدیم-کلسیمدار، بنتونیت آسفیچ از نوع کلسیم-سدیمدار و بنتونیت گلستان از نوع کلسیمی است. سنگ مادر بنتونیتهای مورد بررسی شامل گدازههای اسیدی تا حدواسط (ریوداسیت- داسیت تا آندزیت) و سنگهای آذرآواری (توف-برش) است که دچار دگرسانی متوسط تا شدید شدهاند. محاسبه تغییرات زمینشیمیایی پهنههای بنتونیتی بیانگر کاهش سیلیس، سدیم و پتاسیم و افزایش کلسیم است.
واژه‌های کلیدی: بنتونیت، سربیشه، پردازش ماهوارهای، تغییرات جرمی.
فهرست منابع
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