سامانه مدیریت نشریات علمی دانشگاه دامغان

موسوی, سیده اعظم, ترکیان, اشرف. (1404). زمین دما- فشارسنجی توده نفوذی تکیه (جنوب قروه، استان کردستان): تاکید ویژه بر کاربرد شیمی کانی آمفیبول. مجله زمین شیمی ایران, 29(4), 853-870. doi: 10.52547/ijcm.29.4.853
سیده اعظم موسوی; اشرف ترکیان. "زمین دما- فشارسنجی توده نفوذی تکیه (جنوب قروه، استان کردستان): تاکید ویژه بر کاربرد شیمی کانی آمفیبول". مجله زمین شیمی ایران, 29, 4, 1404, 853-870. doi: 10.52547/ijcm.29.4.853
موسوی, سیده اعظم, ترکیان, اشرف. (1404). 'زمین دما- فشارسنجی توده نفوذی تکیه (جنوب قروه، استان کردستان): تاکید ویژه بر کاربرد شیمی کانی آمفیبول', مجله زمین شیمی ایران, 29(4), pp. 853-870. doi: 10.52547/ijcm.29.4.853
موسوی, سیده اعظم, ترکیان, اشرف. زمین دما- فشارسنجی توده نفوذی تکیه (جنوب قروه، استان کردستان): تاکید ویژه بر کاربرد شیمی کانی آمفیبول. مجله زمین شیمی ایران, 1404; 29(4): 853-870. doi: 10.52547/ijcm.29.4.853

زمین دما- فشارسنجی توده نفوذی تکیه (جنوب قروه، استان کردستان): تاکید ویژه بر کاربرد شیمی کانی آمفیبول

مجله بلورشناسی و کانی شناسی ایران
مقاله 11، دوره 29، شماره 4 - شماره پیاپی 84، دی 1400، صفحه 853-870    اصل مقاله (3.12 M)
شناسه دیجیتال (DOI): 10.52547/ijcm.29.4.853
نویسندگان
سیده اعظم موسوی؛ اشرف ترکیان*
دانشگاه بوعلی سینا
چکیده
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.    
کلیدواژه‌ها
شیمی کانی؛ گریزندگی اکسیژن؛ منیزیوهورنبلند؛ آهکی قلیایی؛ برونبوم؛ تکیه؛ قروه کردستان
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