سامانه مدیریت نشریات علمی دانشگاه دامغان

قریشوندی, حمید, سپاهی, علی اصغر, معانی جو, محمد. (1399). سنگ شناسی، زمین‌شیمی و شیمی‌کانی توده‌‌ نفوذی شهرک (شرق‌تکاب، شمال‌غرب ایران). مجله زمین شیمی ایران, 28(1), 17-36. doi: 10.29252/ijcm.28.1.17
حمید قریشوندی; علی اصغر سپاهی; محمد معانی جو. "سنگ شناسی، زمین‌شیمی و شیمی‌کانی توده‌‌ نفوذی شهرک (شرق‌تکاب، شمال‌غرب ایران)". مجله زمین شیمی ایران, 28, 1, 1399, 17-36. doi: 10.29252/ijcm.28.1.17
قریشوندی, حمید, سپاهی, علی اصغر, معانی جو, محمد. (1399). 'سنگ شناسی، زمین‌شیمی و شیمی‌کانی توده‌‌ نفوذی شهرک (شرق‌تکاب، شمال‌غرب ایران)', مجله زمین شیمی ایران, 28(1), pp. 17-36. doi: 10.29252/ijcm.28.1.17
قریشوندی, حمید, سپاهی, علی اصغر, معانی جو, محمد. سنگ شناسی، زمین‌شیمی و شیمی‌کانی توده‌‌ نفوذی شهرک (شرق‌تکاب، شمال‌غرب ایران). مجله زمین شیمی ایران, 1399; 28(1): 17-36. doi: 10.29252/ijcm.28.1.17

سنگ شناسی، زمین‌شیمی و شیمی‌کانی توده‌‌ نفوذی شهرک (شرق‌تکاب، شمال‌غرب ایران)

مجله بلورشناسی و کانی شناسی ایران
مقاله 2، دوره 28، شماره 1 - شماره پیاپی 77، فروردین 1399، صفحه 17-36    اصل مقاله (2.26 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.28.1.17
نویسندگان
حمید قریشوندی؛ علی اصغر سپاهی* ؛ محمد معانی جو
دانشگاه بوعلی سینا
چکیده
توده نفوذی شهرک در مرز بین استان­های آذربایجان غربی و کردستان قرار دارد. ترکیب سنگ­شناسی این توده نفوذی شامل گرانودیوریت، مونزونیت، مونزودیوریت و مونزوگابرو است که به­ درون واحدهای رسوبی با سن الیگومیوسن و دگرگونی­های با سن کرتاسه و پرکامبرین نفوذ کرده است. بررسی­های شیمی­کانی در سنگ­های گرانودیوریتی تا مونزوگابرویی نشان می­دهد که پلاژیوکلازها دارای ترکیب لابرادوریت تا بیتونیت و کلینوپیروکسن­ها از نوع اوژیت هستند. دما- فشارسنجی بر کانی­های پیروکسن دمای تشکیل این کانی­ها را 900 تا 1250 سانتی­گراد و فشار تبلور کلینوپیروکسن­ها را حدود 6 تا 10 کیلوبار برآورد می­کند. بررسی­های زمین شیمیایی سنگ­کل نشان می­دهد که ماگمای سازنده این سنگ­ها ماهیت متاآلومین و آهکی قلیایی دارد. در طیف چند عنصری بهنجارشده نسبت به کندریت و گوشته اولیه، غنی­شدگی مشخصی از عناصر خاکی نادر سبک LREE نسبت به عناصر خاکی نادر سنگین HREE و تهی­شدگی از Ti، P < /span>، Ta و Nb دیده می­شود که از ویژگی­های بارز سنگ­های کمان­های آتشفشانی مناطق فرورانش است. همچنین براساس نمودارهای مختلف زمین­ساختی ماگمایی، این سنگ­ها در محیط کرانه فعال قاره­ای قرار دارند. بر پایه عناصر خاکی­نادر، ماگمای مادر سنگ­های مورد بررسی احتمالاً از یک گوشته غنی­شده است.     
کلیدواژه‌ها
توده نفوذی شهرک؛ شرق تکاب؛ شیمی‌کانی؛ کرانه فعال قاره‌ای
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