دوره 26، شماره 1 - ( 1-1397 )                   جلد 26 شماره 1 صفحات 195-208 | برگشت به فهرست نسخه ها


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Riyahi Samani, Shabanian Boroujeni, Davoudian Dehkordi. Geochemistry and tectonic setting of granite-gneisses from Abadchi, north of Shahrekord. www.ijcm.ir. 2018; 26 (1) :195-208
URL: http://ijcm.ir/article-1-1060-fa.html
ریاحی سامانی فریبا، شبانیان بروجنی ناهید، داودیان دهکردی علیرضا. زمین‌شیمی و محیط زمین‌ساختی گرانیت گنایس‌های آبادچی، شمال شهرکرد. مجله بلورشناسی و کانی شناسی ایران. 1397; 26 (1) :195-208

URL: http://ijcm.ir/article-1-1060-fa.html


دانشگاه شهرکرد
چکیده:   (503 مشاهده)
توده­ی گرانیت گنایس­ منطقه آبادچی (مجاور سد زاینده‌رود) بخشی از پهنه زمین­ساختی سنندج - سیرجان است. ترکیب کانی‌شناسی این توده‌های گرانیت گنایسی شامل کوارتز، فلدسپات پتاسیم، پلاژیوکلاز، بیوتیت و موسکویت و کانی­های فرعی کدر، زیرکن، آمفیبول و آلانیت است. سنگ‌های گرانیت گنایسی­ مورد بررسی­ تحت تاثیر دگرشکلی دینامیک و دگرنهادی ضعیف سدیمی واقع شده­اند. این سنگ­ها از نظر زمین­شیمی کلسیمی تا آهکی- قلیایی، آهن­دار تا منیزیم­دار، پرآلومین تا کمی متاآلومین و از نوع A تا I هستند. نمودار  REEبهنجارشده به کندریت غنی­شدگیLREE ها را نسبت به HREEها همراه با ناهنجاری منفی Eu نشان می­دهند. این سنگ­ها در نمودارهای عنکبوتی بهنجار شده نسبت به مانتوی اولیه غنی­شدگی نسبی در LILE  وLREE  نسبت به HFSE  را نشان می­دهند که این امر اشاره به سنگ­های ماگمایی وابسته به کمان و محیط­های برخوردی دارد. این گرانیت گنایس در جایگاه زمین­ساختی  پس از برخورد تشکیل شده­اند.    
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نوع مطالعه: پژوهشي | موضوع مقاله: تخصصي
دریافت: ۱۳۹۶/۱۲/۹ | پذیرش: ۱۳۹۶/۱۲/۹ | انتشار: ۱۳۹۶/۱۲/۹

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