دوره 29، شماره 4 - ( 10-1400 )                   جلد 29 شماره 4 صفحات 870-853 | برگشت به فهرست نسخه ها


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Mousavi, Torkian. Geothermobarometry of Tekieh intrusive complex (south of Qorveh, Kurdistan Province): Constraint on using mineral chemistry of amphibole. www.ijcm.ir. 2021; 29 (4) :853-870
URL: http://ijcm.ir/article-1-1686-fa.html
موسوی سیده اعظم، ترکیان اشرف. زمین دما- فشارسنجی توده نفوذی تکیه (جنوب قروه، استان کردستان): تاکید ویژه بر کاربرد شیمی کانی آمفیبول. مجله بلورشناسی و کانی شناسی ایران. 1400; 29 (4) :870-853

URL: http://ijcm.ir/article-1-1686-fa.html


1- دانشگاه بوعلی سینا
چکیده:   (291 مشاهده)
توده نفوذی تکیه در جنوب قروه و در شمال پهنه سنندج-سیرجان قرار دارد. در این توده، برونبوم­های سنگ میزبان گرانیتی ترکیب دیوریت و برونبوم­های سنگ میزبان مونزونیتی ترکیب گابرویی دارند. برونبوم­ها با شکل­های گردشده و بیضوی در سنگ­های میزبان پراکنده هستند، آنها اغلب تماس ناگهانی با سنگ میزبان داشته و از مجموعه کانی­های آذرین تشکیل شده­اند. آمفیبول­ها در هر دو گروه سنگی از نوع کلسیمی بوده و دارای ترکیب منیزیوهورنبلند و اکتینولیت هستند. پلاژیوکلازهای سنگ میزبان و برونبوم ها به ترتیب در گستره ترکیبی الیگوکلاز تا آندزین و الیگوکلاز تا بیتونیت قرار می­گیرند. بر پایه بررسی­های زمین دما-فشار­سنجی بر بلورهای آمفیبول و نیز زوج کانی­های آمفیبول-پلاژیوکلاز، برای سنگ میزبان و برونبوم دیوریتی توده به ترتیب دماهای تقریبی 660-554 و 742-592 درجه سانتیگراد به دست آمد. فشار نیز برای نمونه­های سنگی میزبان و برونبوم دیوریتی این توده نفوذی به ترتیب در گستره 3/0 تا 62/3 و 21/0 تا 8/1 کیلوبار محاسبه شد. گریزندگی اکسیژن در ماگما بالاست که این با ماهیت آهکی قلیایی و شکل­گیری سنگ­ها در محیط فرورانش همخوانی دارد.    
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نوع مقاله: پژوهشي | موضوع مقاله: تخصصي

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