سامانه مدیریت نشریات علمی دانشگاه دامغان

سلیمی, زهره, موذن, محسن, حاجی علی اوغلی, رباب. (1399). سنگ‌نگاری، شیمی کانی‌ و دما- فشارسنجی آمفیبولیت‌های مجموعه‌ی اللهیارلو، استان اردبیل- شمال‌غرب ایران. مجله زمین شیمی ایران, 28(1), 185-198. doi: 10.29252/ijcm.28.1.185
زهره سلیمی; محسن موذن; رباب حاجی علی اوغلی. "سنگ‌نگاری، شیمی کانی‌ و دما- فشارسنجی آمفیبولیت‌های مجموعه‌ی اللهیارلو، استان اردبیل- شمال‌غرب ایران". مجله زمین شیمی ایران, 28, 1, 1399, 185-198. doi: 10.29252/ijcm.28.1.185
سلیمی, زهره, موذن, محسن, حاجی علی اوغلی, رباب. (1399). 'سنگ‌نگاری، شیمی کانی‌ و دما- فشارسنجی آمفیبولیت‌های مجموعه‌ی اللهیارلو، استان اردبیل- شمال‌غرب ایران', مجله زمین شیمی ایران, 28(1), pp. 185-198. doi: 10.29252/ijcm.28.1.185
سلیمی, زهره, موذن, محسن, حاجی علی اوغلی, رباب. سنگ‌نگاری، شیمی کانی‌ و دما- فشارسنجی آمفیبولیت‌های مجموعه‌ی اللهیارلو، استان اردبیل- شمال‌غرب ایران. مجله زمین شیمی ایران, 1399; 28(1): 185-198. doi: 10.29252/ijcm.28.1.185

سنگ‌نگاری، شیمی کانی‌ و دما- فشارسنجی آمفیبولیت‌های مجموعه‌ی اللهیارلو، استان اردبیل- شمال‌غرب ایران

مجله بلورشناسی و کانی شناسی ایران
مقاله 13، دوره 28، شماره 1 - شماره پیاپی 77، فروردین 1399، صفحه 185-198    اصل مقاله (2.03 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.28.1.185
نویسندگان
زهره سلیمی* ؛ محسن موذن؛ رباب حاجی علی اوغلی
دانشگاه تبریز
چکیده
مجموعه افیولیتی- دگرگونی اللهیارلو منسوب به پیش از کرتاسه در مرکز تاقدیس اللهیارلو در شمال غرب ایران و شمال شرق مشگین شهر رخنمون دارد. این مجموعه شامل انواع سنگ­های دگرگونی چون شیست، گنیس، آمفیبولیت و متادیاباز به همراه قطعه­هایی از سرپانتینیت و برش­های زمین­ساختی گابرو، دونیت، مرمر و دیاباز است. آمفیبولیت­های این مجموعه شامل آمفیبولیت و گارنت آمفیبولیت هستند.کانی­های اصلی تشکیل­دهنده­ی آمفیبولیت­ها شامل هورنبلند و پلاژیوکلاز هستند و تیتانیت، زیرکن، کلسیت، اپیدوت و اکسید­های آهن به عنوان کانی­های فرعی حضور دارند. در گارنت آمفیبولیت­ها، افزون بر این کانی­ها، گارنت نیز حضور دارد. بافت­های شکفته بلوری و نخ شکفتی از بافت­های معمول در این سنگ­هاست. بر اساس نتایج تجزیه به روش ریزپردازش الکترونی در آمفیبولیت­ها و گارنت آمفیبولیت­ها، ترکیب آمفیبول­ها دارای گستره ترکیبی منیزیو هورنبلند و چرماکیت، ترکیب پلاژیوکلاز دارای گستره آندزین و آلبیت است و در گارنت آمفیبولیت­ها، گارنت ترکیب غنی از آلماندین دارد. بر اساس تغییرات مقدار عنصر Ti نسبت به Alt، آمفیبول­های مورد بررسی در آمفیبولیت­های مجموعه دگرگونی اللهیارلو، از آمفیبول­های فشار متوسط هستند. نتایج دما- فشارسنجی این سنگ­ها بر اساس شیمی آمفیبول، گارنت و پلاژیوکلاز بیانگر فشار (p) حدود 8 کیلوبار و دمای (T) حدود 600 درجه سانتیگراد است. بنابراین با روند دگرگونی بارووین P/T متوسط که نشانگر مناطق ضخیم شدگی پوسته ای (جزایر قوسی و یا قوس آتشفشانی) و یا مناطق برخوردی است همخوانی دارد.     
کلیدواژه‌ها
شیمی کانی‌؛ دما- فشارسنجی؛ آمفیبولیت؛ اللهیارلو؛ شمال‌غرب ایران
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