سامانه مدیریت نشریات علمی دانشگاه دامغان

فضیلت, آسیه, صادقیان, محمود. (1399). بررسی تغییرات کانی‌شناسی و ریزساختی گرانیت‌های چاه‌زرد (شرق‌جندق) طی میلونیت‌زایی براساس روش ناهمسانگردی پذیرفتاری مغناطیسی (AMS). مجله زمین شیمی ایران, 28(1), 199-216. doi: 10.29252/ijcm.28.1.199
آسیه فضیلت; محمود صادقیان. "بررسی تغییرات کانی‌شناسی و ریزساختی گرانیت‌های چاه‌زرد (شرق‌جندق) طی میلونیت‌زایی براساس روش ناهمسانگردی پذیرفتاری مغناطیسی (AMS)". مجله زمین شیمی ایران, 28, 1, 1399, 199-216. doi: 10.29252/ijcm.28.1.199
فضیلت, آسیه, صادقیان, محمود. (1399). 'بررسی تغییرات کانی‌شناسی و ریزساختی گرانیت‌های چاه‌زرد (شرق‌جندق) طی میلونیت‌زایی براساس روش ناهمسانگردی پذیرفتاری مغناطیسی (AMS)', مجله زمین شیمی ایران, 28(1), pp. 199-216. doi: 10.29252/ijcm.28.1.199
فضیلت, آسیه, صادقیان, محمود. بررسی تغییرات کانی‌شناسی و ریزساختی گرانیت‌های چاه‌زرد (شرق‌جندق) طی میلونیت‌زایی براساس روش ناهمسانگردی پذیرفتاری مغناطیسی (AMS). مجله زمین شیمی ایران, 1399; 28(1): 199-216. doi: 10.29252/ijcm.28.1.199

بررسی تغییرات کانی‌شناسی و ریزساختی گرانیت‌های چاه‌زرد (شرق‌جندق) طی میلونیت‌زایی براساس روش ناهمسانگردی پذیرفتاری مغناطیسی (AMS)

مجله بلورشناسی و کانی شناسی ایران
مقاله 14، دوره 28، شماره 1 - شماره پیاپی 77، فروردین 1399، صفحه 199-216    اصل مقاله (8.94 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.28.1.199
نویسندگان
آسیه فضیلت؛ محمود صادقیان*
دانشگاه صنعتی شاهرود
چکیده
توده گرانیتی چاه­زرد با سن 2/3± 4/535 میلیون­سال (تعیین شده به روش  U-Pbبر روی زیرکن) به­ درون مجموعه دگرگونی جندق - عروسان نفوذ کرده و طی رخدادهای ­بعدی به­شدت میلونیتی­شده­است. این توده گرانیتی، برای نخستین بار براساس روش ناهمسانگردی پذیرفتاری مغناطیسی (AMS) بررسی شده است. مقدار میانگین پذیرفتاری مغناطیسی (Km) بیوتیت­گرانیت­ها (سازنده اصلی پیکره توده گرانیتی چاه زرد) µSI 112 است. بیوتیت مهمترین حامل ­مغناطیسی در بیوتیت­گرانیت­هاست. طی میلونیت­زایی، حجم قابل­توجهی از بیوتیت­ها به مسکوویت تحوّل پیدا کرده و در نتیجه، مقادیر Km سنگ­های دربرگیرنده آنها به شدت کاهش یافته است. خطواره­ها و برگواره­های مغناطیسی این توده گرانیتی به ترتیب، بیشتر دارای میل و شیب بسیار کمی هستند، شواهد صحرایی نیز این امر را تأیید می­کند. خطواره­های مغناطیسی، بیشتر به­سمت شمال­غرب آرایش یافته­اند. از آن­جا که شدت میلونیتی­شدن بسیار زیاد است، ریزساخت­های دستخوش تنش­های زمین­ساختی، بر ریزساخت­های ماگمایی غلبه پیدا کرده و آن­ها را به طور کامل مخدوش کرده­اند.
کلیدواژه‌ها
گرانیت؛ ناهمسانگردی پذیرفتاری مغناطیسی؛ میلونیت‌زایی؛ چاه‌زرد؛ جندق
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