سامانه مدیریت نشریات علمی دانشگاه دامغان

ترکیان, اشرف, شیرمحمدی, زهرا, جعفری, سیده راضیه. (1402). سنگ‌نگاری، شیمی کانی و زمین‌دما-فشارسنجی مجموعهی دگرگونی گرمخانی-میهم (قروه-کردستان). مجله زمین شیمی ایران, 31(3), 479-496. doi: 10.61186/ijcm.31.3.479
اشرف ترکیان; زهرا شیرمحمدی; سیده راضیه جعفری. "سنگ‌نگاری، شیمی کانی و زمین‌دما-فشارسنجی مجموعهی دگرگونی گرمخانی-میهم (قروه-کردستان)". مجله زمین شیمی ایران, 31, 3, 1402, 479-496. doi: 10.61186/ijcm.31.3.479
ترکیان, اشرف, شیرمحمدی, زهرا, جعفری, سیده راضیه. (1402). 'سنگ‌نگاری، شیمی کانی و زمین‌دما-فشارسنجی مجموعهی دگرگونی گرمخانی-میهم (قروه-کردستان)', مجله زمین شیمی ایران, 31(3), pp. 479-496. doi: 10.61186/ijcm.31.3.479
ترکیان, اشرف, شیرمحمدی, زهرا, جعفری, سیده راضیه. سنگ‌نگاری، شیمی کانی و زمین‌دما-فشارسنجی مجموعهی دگرگونی گرمخانی-میهم (قروه-کردستان). مجله زمین شیمی ایران, 1402; 31(3): 479-496. doi: 10.61186/ijcm.31.3.479

سنگ‌نگاری، شیمی کانی و زمین‌دما-فشارسنجی مجموعهی دگرگونی گرمخانی-میهم (قروه-کردستان)

مجله بلورشناسی و کانی شناسی ایران
مقاله 5، دوره 31، شماره 3 - شماره پیاپی 91، مهر 1402، صفحه 479-496    اصل مقاله (4.73 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.61186/ijcm.31.3.479
نویسندگان
اشرف ترکیان* 1؛ زهرا شیرمحمدی2؛ سیده راضیه جعفری3
1دانشگاه گروه زمین‌شناسی، دانشکده علوم پایه، دانشگاه بوعلی سینا، همدان
2گروه زمین‌شناسی، دانشکده علوم پایه، دانشگاه بوعلی سینا، همدان
3گروه زمین شناسی، دانشکده علوم، دانشگاه پیام نور، تهران
چکیده
منطقه گرمخانی - میهم در جنوب ­شرق شهرستان قروه و بخش شمال­غرب پهنه سنندج-سیرجان واقع است. سنگ­های این منطقه شامل تنوعی از سنگ­های دگرگونی ناحیه­ای و مجاورتی هستند. داده­های ریزپردازشی نشان می­دهد که آمفیبول­ها از نوع مگنزیوهورنبلند، پلاژیوکلازها از نوع آندزین و آلبیت، بیوتیت­ از زیرمجموعه سیدروفیلیت، میکای سفید از نوع موسکویت و اپیدوت نیز از زیر مجموعه کلینوزوئیزیت هستند. بر اساس شیمی آمفیبول­ها، سری ماگمایی ماگمای سازنده آن­ها، نیمه قلیایی و محیط زمین ساختی آن ابرفرورانشی است. برآوردهای زمین­دما-فشارسنجی کانی­های آمفیبول و پلاژیوکلاز در آمفیبول­شیست­ها گستره دمایی 464 تا 570 درجه سانتی­گراد و فشار 3 تا 6/5 کیلوبار را نشان می­دهد که بیانگر گذر از رخساره شیست سبز به آمفیبولیت است.    
کلیدواژه‌ها
شیمی کانی؛ شیست سبز؛ دگرگونی ناحیه‌ای؛ دگرگونی مجاورتی؛ زون سنندج- سیرجان
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