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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
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
سیدسعید محمدی* 
1، ملیحه نخعی2
1، ملیحه نخعی2
1- گروه زمین‌شناسی، دانشکده علوم، دانشگاه بیرجند، بیرجند، ایران
2- گروه مهندسی معدن، دانشکده عمران، معدن و شیمی، دانشگاه صنعتی بیرجند، بیرجند، ایران
2- گروه مهندسی معدن، دانشکده عمران، معدن و شیمی، دانشگاه صنعتی بیرجند، بیرجند، ایران
چکیده: (1131 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.
واژه‌های کلیدی: بازالت، کریزولیت، خاستگاه پریدوتیتی، کمان قاره، پدران، لوت.
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