سامانه مدیریت نشریات علمی دانشگاه دامغان

قاسمی سیانی, مجید, مهرابی, بهزاد. (1399). زمین‌دماسنجی پهنه‌های اسکارنی ناهنجاری کانسار دردوی، منطقه معدنی آهن سنگان. مجله زمین شیمی ایران, 28(1), 125-140. doi: 10.29252/ijcm.28.1.125
مجید قاسمی سیانی; بهزاد مهرابی. "زمین‌دماسنجی پهنه‌های اسکارنی ناهنجاری کانسار دردوی، منطقه معدنی آهن سنگان". مجله زمین شیمی ایران, 28, 1, 1399, 125-140. doi: 10.29252/ijcm.28.1.125
قاسمی سیانی, مجید, مهرابی, بهزاد. (1399). 'زمین‌دماسنجی پهنه‌های اسکارنی ناهنجاری کانسار دردوی، منطقه معدنی آهن سنگان', مجله زمین شیمی ایران, 28(1), pp. 125-140. doi: 10.29252/ijcm.28.1.125
قاسمی سیانی, مجید, مهرابی, بهزاد. زمین‌دماسنجی پهنه‌های اسکارنی ناهنجاری کانسار دردوی، منطقه معدنی آهن سنگان. مجله زمین شیمی ایران, 1399; 28(1): 125-140. doi: 10.29252/ijcm.28.1.125

زمین‌دماسنجی پهنه‌های اسکارنی ناهنجاری کانسار دردوی، منطقه معدنی آهن سنگان

مجله بلورشناسی و کانی شناسی ایران
مقاله 9، دوره 28، شماره 1 - شماره پیاپی 77، فروردین 1399، صفحه 125-140    اصل مقاله (6 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.28.1.125
نویسندگان
مجید قاسمی سیانی* ؛ بهزاد مهرابی
دانشگاه خوارزمی
چکیده
کانسار اسکارن آهن دردوی در بخش مرکزی منطقه معدنی سنگان در شمال شرق ایران واقع شده است. در این پژوهش،  دمای تشکیل پهنه­های اسکارنی آن با استفاده از برخی زمین­دماسنج­ها برآورد شده است. مهمترین­ کانی­های دگرگونی در پهنه­های اسکارنی پیشرونده و پسرونده شامل گارنت، کلینوپیروکسن، ترمولیت-اکتینولیت، آمفیبول، کلریت، اپیدوت، فلدسپار، فلوگوپیت و دولومیت هستند. زمین­دماسنج دوفلدسپار نشان داد که پهنه درون­اسکارن در گرانیت سرنوسر در دماهای بین 635 تا 725 درجه سانتیگراد تشکیل شده که با دماهای بدست آمده از میانبارهای سیال همخوانی ندارد. بر اساس زمین­دماسنج گارنت-کلینوپیروکسن، دماهای 300 تا 505 درجه سانتیگراد برای دگرگونی اسکارن پیشرونده بدست آمد. زمین­دماسنج کلریت و آمفیبول کلسیمی در پهنه پسرونده به ترتیب دماهای تشکیل بین 200 تا 290 و 200 تا 300 درجه سانتیگراد را نشان داد. نتایج زمین­دماسنج پهنه­های اسکارنی پیشرونده و پسرونده با نتایج سیال­های درگیر همخوانی دارند. دماهای بدست آمده از میانبارهای سیال و زمین­دماسنج پهنه­های اسکارن پیشرونده و پسرونده نشان داد که دماهای تشکیل اسکارن دگرگونی مجاورتی کمتر از 600 درجه سانتیگراد است که با رخساره دگرگونی هورنبلند-هورنفلس همخوانی دارد.    
کلیدواژه‌ها
منطقه معدنی آهن سنگان؛ ناهنجاری دردوی؛ زمین‌دماسنجی؛ پهنه‌های اسکارن؛ سرنوسر
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