سامانه مدیریت نشریات علمی دانشگاه دامغان

پورمرادیان برفه, علیرضا, ابراهیمی, محمد, نباتیان, قاسم, مرادیان, عباس, عباسلو, زهرا. (1404). سنگ‌شناسی سنگ‌های آتشفشانی منطقه کاریک، شرق معدن مس میدوک. مجله زمین شیمی ایران, 29(4), 733-746. doi: 10.52547/ijcm.29.4.733
علیرضا پورمرادیان برفه; محمد ابراهیمی; قاسم نباتیان; عباس مرادیان; زهرا عباسلو. "سنگ‌شناسی سنگ‌های آتشفشانی منطقه کاریک، شرق معدن مس میدوک". مجله زمین شیمی ایران, 29, 4, 1404, 733-746. doi: 10.52547/ijcm.29.4.733
پورمرادیان برفه, علیرضا, ابراهیمی, محمد, نباتیان, قاسم, مرادیان, عباس, عباسلو, زهرا. (1404). 'سنگ‌شناسی سنگ‌های آتشفشانی منطقه کاریک، شرق معدن مس میدوک', مجله زمین شیمی ایران, 29(4), pp. 733-746. doi: 10.52547/ijcm.29.4.733
پورمرادیان برفه, علیرضا, ابراهیمی, محمد, نباتیان, قاسم, مرادیان, عباس, عباسلو, زهرا. سنگ‌شناسی سنگ‌های آتشفشانی منطقه کاریک، شرق معدن مس میدوک. مجله زمین شیمی ایران, 1404; 29(4): 733-746. doi: 10.52547/ijcm.29.4.733

سنگ‌شناسی سنگ‌های آتشفشانی منطقه کاریک، شرق معدن مس میدوک

مجله بلورشناسی و کانی شناسی ایران
مقاله 2، دوره 29، شماره 4 - شماره پیاپی 84، دی 1400، صفحه 733-746    اصل مقاله (5.77 M)
شناسه دیجیتال (DOI): 10.52547/ijcm.29.4.733
نویسندگان
علیرضا پورمرادیان برفه1؛ محمد ابراهیمی* 1؛ قاسم نباتیان1؛ عباس مرادیان2؛ زهرا عباسلو3
1دانشگاه زنجان
2دانشگاه شهید باهنر کرمان
3معدن مس میدوک
چکیده
پیرامون روستای کاریک در شرق معدن مس میدوک، سنگ­های آتشفشانی (بازالت آندزیتی، آندزیت، داسیت و ریولیت) و سنگ­های آذرآواری (آگلومرا و توف) ائوسن رخنمون دارند. این سنگ‌ها با تعدادی دایک‌ با ترکیبب آندزیتی قطع شده‌اند. بافت­های اصلی سنگ­های آتشفشانی پورفیری و جریانی هستند. کانی­های پلاژیوکلاز، فلدسپار قلیایی، کوارتز، کلینوپیروکسن، آمفیبول، بیوتیت و کانی‌های کدر در سنگ‌های مورد بررسی به صورت درشت‌بلور و بلورهای ریز وجود دارند. همچنین، فلدسپار (بیشتر پلاژیوکلاز) به صورت ریزبلورهای میله­ای جهت‌یافته دیده می‌شود. گاهی در درشت‌بلورهای پلاژیوکلاز، بافت­های غیرتعادلی چون بافت غربالی، تحلیل‌یافتگی و منطقه‌بندی مشاهده می‌گردند. کوارتزها لبه­های تحلیل یافته دارند. آمفیبول­ها و بیوتیت­ها از لبه‌ها به اکسیدهای آهن و تیتانیم تبدیل شده‌اند. تشکیل این بافت­ها را می­توان به فرایندهایی چون آمیختگی ماگمایی، تغییرات فشار بخار آب و کاهش فشار ناشی از صعود سریع ماگما مربوط دانست. سنگ­های آتشفشانی منطقه کاریک از سری ماگمایی آهکی قلیایی و بیشتر متاآلومین هستند. نمودارهای چندعنصری سنگ‌های مورد بررسی بهنجار شده‌ نسبت به کندریت و گوشته اولیه دارای ناهنجاری منفی عناصر با شدت میدان بالا چون P < /span>، Nb،Ta  و Ti هستند که از ویژگی‌های ماگماهای وابسته به مناطق فرورانش است. ناهنجاری مثبت شدید Pb در سنگ‌های مورد بررسی ناشی از آلایش پوسته‌ای است. الگوی عناصر خاکی نادر بهنجار شده به کندریت سنگ­های آذرین منطقه کاریک به نسبت هموار و دارای غنی‌شدگی عناصر خاکی نادر سبک (LREE) نسبت به عناصر خاکی نادر سنگین بوده که به احتمال بسیار به دلیل فراوانی LREE ها در خاستگاه و یا آلایش پوسته‌ای است. بر اساس شواهد سنگ‌شناسی و زمین شیمیایی، سنگ‌های آتشفشانی منطقه کاریک در یک محیط کمان فعال کرانه قاره‌ای و بر اثر فرورانش سنگ کره اقیانوسی نئوتتیس به زیر خرده‌قاره ایران مرکزی تشکیل شده‌اند.    
کلیدواژه‌ها
سنگ‌‌نگاری؛ زمین شیمی؛ سنگ‌های آتشفشانی؛ کاریک؛ کرمان؛ پهنه ارومیه- دختر
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