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آهنگری, معصومه. (1397). توزیع عناصر کمیاب و خاکی نادر در میان فازهای دگرگونی و کلینوپیروکسن‌های باقیمانده در اپیدوت- آمفیبولیت‌های شمال ارومیه- شمال‌غرب ایران. مجله زمین شیمی ایران, 26(2), 287-300. doi: 10.29252/ijcm.26.2.287
معصومه آهنگری. "توزیع عناصر کمیاب و خاکی نادر در میان فازهای دگرگونی و کلینوپیروکسن‌های باقیمانده در اپیدوت- آمفیبولیت‌های شمال ارومیه- شمال‌غرب ایران". مجله زمین شیمی ایران, 26, 2, 1397, 287-300. doi: 10.29252/ijcm.26.2.287
آهنگری, معصومه. (1397). 'توزیع عناصر کمیاب و خاکی نادر در میان فازهای دگرگونی و کلینوپیروکسن‌های باقیمانده در اپیدوت- آمفیبولیت‌های شمال ارومیه- شمال‌غرب ایران', مجله زمین شیمی ایران, 26(2), pp. 287-300. doi: 10.29252/ijcm.26.2.287
آهنگری, معصومه. توزیع عناصر کمیاب و خاکی نادر در میان فازهای دگرگونی و کلینوپیروکسن‌های باقیمانده در اپیدوت- آمفیبولیت‌های شمال ارومیه- شمال‌غرب ایران. مجله زمین شیمی ایران, 1397; 26(2): 287-300. doi: 10.29252/ijcm.26.2.287

توزیع عناصر کمیاب و خاکی نادر در میان فازهای دگرگونی و کلینوپیروکسن‌های باقیمانده در اپیدوت- آمفیبولیت‌های شمال ارومیه- شمال‌غرب ایران

مجله بلورشناسی و کانی شناسی ایران
مقاله 3، دوره 26، شماره 2 - شماره پیاپی 72، تیر 1397، صفحه 287-300    اصل مقاله (7.83 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.26.2.287
نویسنده
معصومه آهنگری*
دانشگاه ارومیه
چکیده
 مقدار عناصر خاکی نادر و کمیاب موجود در کانی‌های آمفیبول، پلاژیوکلاز، کانی‌های گروه اپیدوت (زوئیزیت و کلینوزوئیزیت) و کلینوپیروکسن‌های باقیمانده از سنگ اولیه در اپیدوت- آمفیبولیت‌های شمال ارومیه به صورت برجا به روش طیف­سنجی جرمی پلاسمای جفت شده القایی لیزری (LA-ICP-MS) جهت بررسی توزیع عناصر کمیاب در کانی­های سنگ­های دگرگونی و کلینوپیروکسن­های باقیمانده از سنگ اولیه، تعیین شدند. در این سنگ‌ها عناصر سازگار (Sc، V، Ni و Cr)، عناصر با شدت میدان بالا یا HFSE (Ti، Ta، Hf و Nb) و عناصر خاکی نادر متوسط (MREE) در آمفیبول، عناصر خاکی نادر سبک (LREE) و عناصر سنگ دوست بزرگ یون (LILE) در پلاژیوکلاز و عناصر خاکی نادر سنگین (HREE) به همراه Eu در کانی‌های گروه اپیدوت تمرکز یافته‌اند. روند مشاهده شده برای عناصر خاکی نادر در کانی‌های گروه اپیدوت برخلاف روند معمول در این کانی‌ها در دیگر نقاط جهان است. بررسی زمین­شیمی عناصر کمیاب و خاکی نادر در این کانی‌ها نشانگر غنی‌شدگی HREE و MREE در مقایسه با LREE در ساختار این کانی‌هاست. مقایسه فراوانی عناصر خاکی نادر و کمیاب بین آمفیبول و کلینوپیروکسن‌های باقیمانده از سنگ اولیه بیانگر تشابه نسبی این عناصر برای این کانی‌هاست. این امر به احتمال زیاد بیانگر به ارث رسیدن ویژگی­های زمین­شیمیایی آمفیبول از کلینوپیروکسن‌های اولیه است.    
کلیدواژه‌ها
ضریب توزیع عناصر کمیاب؛ آمفیبول؛ پلاژیوکلاز؛ کانی‌های گروه اپیدوت؛ اپیدوت- آمفیبولیت؛ شمال ارومیه
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