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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
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) :853-870
سیده اعظم موسوی1 
، اشرف ترکیان* 1
، اشرف ترکیان* 1
1- دانشگاه بوعلی سینا
چکیده: (1034 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.
واژه‌های کلیدی: شیمی کانی، گریزندگی اکسیژن، منیزیوهورنبلند، آهکی قلیایی، برونبوم، تکیه، قروه کردستان.
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