دوره 32، شماره 1 - ( 1-1403 )                   جلد 32 شماره 1 صفحات 126-113 | برگشت به فهرست نسخه ها


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Riyahi F, Shabanian N, Davoudian A. Fractal analysis of quartz grain boundary sutures gneissic granite of Abadchi, north of Shahrekord. www.ijcm.ir 2024; 32 (1) :113-126
URL: http://ijcm.ir/article-1-1854-fa.html
ریاحی فریبا، شبانیان ناهید، داودیان علیرضا. تعیین شرایط دگرگونی برگشتی دایک‌های متادلریتی مجموعه دگرگونی شمال شهرکرد، براساس شیمی کانیایی کلریت و ماکل دگرشکلی کلسیت. مجله بلورشناسی و کانی شناسی ایران. 1403; 32 (1) :113-126

URL: http://ijcm.ir/article-1-1854-fa.html


1- دانشکده منابع طبیعی و علوم زمین، دانشگاه شهرکرد، شهرکرد، ایران
چکیده:   (990 مشاهده)
دایک­های متادلریتی مورد بررسی در شمال استان چهارمحال و بختیاری و در کرانه رودخانه زاینده رود و در مجموعه دگرگونی شمال شهرکرد رخنمون یافته­اند. منطقه مورد بررسی در پهنه زمین­ساختی سنندج-سیرجان قرار دارد. بافت­های اصلی بین دانه­ای، پوست ماری و نیمه­پوست­ماری در این سنگ­ها دیده می­شود. کانی­های اصلی دایک­های متادلریتی پلاژیوکلاز، کلینوپیروکسن و آمفیبول بوده و کانی­های کلریت، کلسیت، سریسیت، اپیدوت، کلینوزوئزیت، اکتینولیت، لوکوکسن و بیوتیت کانی­های فرعی و ثانویه هستند. با توجه به بافت و نتایج کانی­شناسی، این سنگ­ها شواهد یک دگرگونی ناحیه­ای برگشتی رخساره شیست سبز را آشکار می­سازند. با توجه به بررسی­های انجام شده بر کانی کلسیت، ماکل­های دگرشکلی از نوع III  و IV هستند. این ماکل­های دگرشکلی بازتبلور پویای کلسیت در گستره دمایی 200 تا بیش از °C250 را نشان می­دهند. همچنین براساس زمین­دماسنجی بر کانی کلریت این سنگ­ها، دمای تشکیل کلریت از 370 تا 246 درجه سانتی­گراد متغیر است که با دمای دگرشکلی در ماکل­های کلسیت همخوانی دارد.     
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نوع مقاله: پژوهشي | موضوع مقاله: تخصصي

فهرست منابع
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