دوره 30، شماره 1 - ( 1-1401 )
جلد 30 شماره 1 صفحات 28-15 |
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Asadpou, Ahangari. Petrography, geochemistry and source of Ghazan Plio-Quaternary basalts, NW Urmia. www.ijcm.ir 2022; 30 (1) :15-28
URL: http://ijcm.ir/article-1-1710-fa.html
URL: http://ijcm.ir/article-1-1710-fa.html
فتاحی رامین، اسدپور منیژه، آهنگری معصومه. سنگ‌نگاری، زمینشیمی و خاستگاه بازالت‌های پلیوکواترنر غازان، شمال غرب ارومیه. مجله بلورشناسی و کانی شناسی ایران. 1401; 30 (1) :15-28
رامین فتاحی1، منیژه اسدپور* 
1، معصومه آهنگری1
1، معصومه آهنگری1
1- دانشگاه ارومیه
چکیده: (1394 مشاهده)
سنگهای آتشفشانی پلیوکواترنر در شمالیترین بخش پهنه سنندج – سیرجان، در شمال غرب ارومیه رخنمون گستردهای دارند. بلورهای اولیوین+ پیروکسن± پلاژیوکلاز فاز اصلی کانیایی هستند که هم بصورت درشت بلور و هم ریز بلور با کانیهای فرعی دیگر در متن سنگ وجود دارند. این سنگها بافتهای پورفیری، ریزسنگی پورفیری، شیشه ای پورفیری، انبوهه پورفیری و حفرهای دارند. از نظر زمینشیمی، سنگ خاستگاه این سنگها با طیف ترکیبی تراکیبازالت تا تراکیآندزیت بازالت وابسته به سریهای قلیایی هستند. نمودارهای عنکبوتی عناصر کمیاب بهنجار شده به گوشته و کندریت غنی شدگی در عناصر خاکی نادر سبک (LREE) و عناصر سنگ دوست بزرگ یون (LILE) نسبت به عناصر نادر خاکی سنگین (HREE) و عناصر با شدت میدان بالا HFSE نشان میدهند. در این نمودارها، بیهنجاری منفی در Nb، Ta، P، Rb، Zr و Ti و بیهنجاری مثبت در Pb، La، U، Nd،Th ، Yb و Cs وجود دارد. این ویژگیها بهمراه نمودارهای زمینساختی نشان میدهند که فعالیت ماگمایی پلیو-کواترنر غازان در پهنههای کمانهای ماگمایی پس از برخوردی رخ دادهاند.
فهرست منابع
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