دوره 28، شماره 3 - ( 7-1399 )
جلد 28 شماره 3 صفحات 658-645 |
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Shahrokhi. Mineralogy and geochemistry of tourmalines in Malmir Area
(East of Doroud- Iran). www.ijcm.ir 2020; 28 (3) :645-658
URL: http://ijcm.ir/article-1-1519-fa.html
URL: http://ijcm.ir/article-1-1519-fa.html
شاهرخی سید وحید. کانی‌شناسی و زمین‌شیمی تورمالینهای ناحیه مالمیر (شرق دورود- ایران). مجله بلورشناسی و کانی شناسی ایران. 1399; 28 (3) :645-658
دانشگاه آزاد اسلامی، خرم‌آباد
چکیده: (1458 مشاهده)
ناحیه مالمیر در پهنه دگرگونه سنندج-سیرجان و در شرق شهرستان دورود قرار دارد. کهن‌ترین نهشته‌ها شامل توالی به نسبت یکنواخت اسلیت و فیلیت با رگه و رگچه‌های سیلیسی است. مهمترین واحد زمین‌شناسی موجود توده گرانیتوئیدی مالمیر به سن ژوراسیک میانی است. تجزیه به روش ریزپردازش از تورمالینهای موجود در پگماتیت‌ها و رگه‌های کوارتز-تورمالین نشان می‌دهد که همه تورمالینها در گستره شورل-فوئیتیت با تمرکز بیشتر در منطقه شورلیت قرار دارند. رخدادهای بسیار تورمالین در واحد گرانیتی، خودشکلی و نبود منطقه‌بندی شیمیایی، بالا بودن مقدار Al و Fe/Fe+Mg و نقص در جایگاه X تورمالینها بیانگر ماگمایی بودن آنهاست. بنابراین تورمالینهای مورد بررسی وابسته به محیط‌های گرانیتی هستند و بوسیله یک سیال گرمابی با خاستگاه ماگمایی بوجود آمده‌اند. نتایج بیانگر بالا بودن نسبی مقدار Fe#، و نزدیک بودن ناحیه تشکیل تورمالینها با منبع تغذیه کننده سیال و فاصله کم با توده نفوذی هستند.
فهرست منابع
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