دوره 27، شماره 2 - ( 4-1398 )                   جلد 27 شماره 2 صفحات 385-400 | برگشت به فهرست نسخه ها


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Shahrokhi S V, Delfani H. Geochemistry and source determination of tourmalines in Mollataleb Area (North of Aligoudarz- Iran). www.ijcm.ir. 2019; 27 (2) :385-400
URL: http://ijcm.ir/article-1-1273-fa.html
شاهرخی سید وحید، دلفانی حسین. بررسی‌شیمی کانی و تعیین خاستگاه تورمالینهای ناحیه ملاطالب (شمال الیگودرز- ایران). مجله بلورشناسی و کانی شناسی ایران. 1398; 27 (2) :385-400

URL: http://ijcm.ir/article-1-1273-fa.html


دانشگاه آزاد اسلامی
چکیده:   (221 مشاهده)
ناحیه ملاطالب در شمال شهرستان الیگودرز و در پهنه دگرگونه سنندج-سیرجان قرار دارد. قدیمی‌ترین نهشته‌های موجود شامل توالی نسبتاً یکنواخت اسلیت و شیست با رگه و رگچه‌های سیلیسی به همراه هورنفلس‌های سیاه رنگ و ماسه‌سنگ‌های دگرگون‌شده است. پیدایش و نفوذ توده‌های گرانیتوئیدی ناحیه الیگودرز در زمان ژوراسیک میانی در درون شیست‌ها مهمترین رخداد زمین‌شناسی در این ناحیه است. تجزیه به روش ریزپردازش الکترونی (نقطه‌ای) از تورمالین‌های موجود در پگماتیت‌ها، رگه‌های آپلیتی-پگماتیتی تورمالین‌دار، تورمالین‌های گرهکی و رگه‌های کوارتز-تورمالین نشان می‌دهد که همه تورمالین‌ها در گستره بین شورل-فوئیتیت با تمرکز بیشتر در منطقه شورلیت قرار گرفته‌اند. رخدادهای متعدد و فراوان تورمالین در واحد گرانیتی، خودشکلی و عدم وجود پهنه‌بندی شیمیائی، بالا بودن مقدار Al و Fe/Fe+Mg، و همچنین تهیجای X در تورمالین‌‌ها قابل مشاهده بوده و بیانگر ماگمایی بودن آنهاست. بنابراین تورمالین‌های مورد بررسی وابسته به محیط‌های گرانیتی بوده و بوسیله یک سیال گرمابی با خاستگاه ماگمایی بوجود آمده‌اند.     
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نوع مطالعه: پژوهشي | موضوع مقاله: تخصصي
دریافت: ۱۳۹۸/۳/۱۲ | پذیرش: ۱۳۹۸/۳/۱۲ | انتشار: ۱۳۹۸/۳/۱۲

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