دوره 31، شماره 4 - ( 10-1402 )                   جلد 31 شماره 4 صفحات 756-737 | برگشت به فهرست نسخه ها


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Mohammadi S S, nakhaei M. Petrography, olivine chemistry, geochemistry and origin of basalts of the Pedaran area (Southeast of Birjand). www.ijcm.ir 2023; 31 (4) :737-756
URL: http://ijcm.ir/article-1-1874-fa.html
محمدی سیدسعید، نخعی ملیحه. سنگ‌نگاری، شیمی الیوین، زمین‌شیمی و خاستگاه بازالت‌های منطقه پدران (جنوب شرق بیرجند). مجله بلورشناسی و کانی شناسی ایران. 1402; 31 (4) :737-756

URL: http://ijcm.ir/article-1-1874-fa.html


1- گروه زمین‌شناسی، دانشکده علوم، دانشگاه بیرجند، بیرجند، ایران
2- گروه مهندسی معدن، دانشکده عمران، معدن و شیمی، دانشگاه صنعتی بیرجند، بیرجند، ایران
چکیده:   (751 مشاهده)
در کرانه جنوب شرقی روستای پدران در40 کیلومتری جنوب شرق بیرجند، توده­های بازالتی دربردارنده درشت بلور­های الیوین و زمینه ریزدانه شامل پیروکسن، پلاژیوکلاز و کانی کدر رخنمون دارد. بر اساس نتایج تجزیه ریزپردازشی پرتوی ایکس، کانی الیوین دارای ترکیب Fo75-87 Fa13-26 و از نوع کریزولیت است. نسبت­های Ni/Mg وMn/Fe در کانی الیوین بیانگر خاستگاه پریدوتیتی برای مذاب سازنده بازالت هستند. این سنگ­ها بر پایه ویژگی­های زمین شیمیایی عناصر اصلی، ماهیت قلیایی (نزدیک به نیمه قلیایی) دارند. عناصر با شدت میدان بالا (HFSE)، چون Nb، P،Zr  و Ti، بی­هنجاری منفی نشان می­دهند که بیانگر تشکیل آن­ها درمنـاطق فـرورانش اسـت. ماگمای سازنده بازالت­های پدران از منطقه تحولی بین فازهای اسپینل و گارنت لرزولیت در عمق حدود70 کیلومتر شکل گرفته است. نمودارهای تعیین محیط زمین­ساختی برپایه عناصر نادر نشان می­دهند که نمونه­ها در قلمرو بازالت­های آهکی­قلیایی قرار دارند و وابسته به کمان قاره­ای هستند.
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نوع مقاله: پژوهشي | موضوع مقاله: تخصصي

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