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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
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
فریبا ریاحی1 
، ناهید شبانیان* 1، علیرضا داودیان1
، ناهید شبانیان* 1، علیرضا داودیان1
1- دانشکده منابع طبیعی و علوم زمین، دانشگاه شهرکرد، شهرکرد، ایران
چکیده: (1368 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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