سامانه مدیریت نشریات علمی دانشگاه دامغان

نادرمزرجی, سمانه, کریم‌پور, محمدحسن, ملکزاده شفارودی, آزاده. (1397). سنگ‌‌نگاری، زمین‌شیمی و جایگاه زمین‌ساختی واحدهای آتشفشانی منطقه شاه سلطان علی (جنوب غربی بیرجند). مجله زمین شیمی ایران, 26(2), 369-382. doi: 10.29252/ijcm.26.2.369
سمانه نادرمزرجی; محمدحسن کریم‌پور; آزاده ملکزاده شفارودی. "سنگ‌‌نگاری، زمین‌شیمی و جایگاه زمین‌ساختی واحدهای آتشفشانی منطقه شاه سلطان علی (جنوب غربی بیرجند)". مجله زمین شیمی ایران, 26, 2, 1397, 369-382. doi: 10.29252/ijcm.26.2.369
نادرمزرجی, سمانه, کریم‌پور, محمدحسن, ملکزاده شفارودی, آزاده. (1397). 'سنگ‌‌نگاری، زمین‌شیمی و جایگاه زمین‌ساختی واحدهای آتشفشانی منطقه شاه سلطان علی (جنوب غربی بیرجند)', مجله زمین شیمی ایران, 26(2), pp. 369-382. doi: 10.29252/ijcm.26.2.369
نادرمزرجی, سمانه, کریم‌پور, محمدحسن, ملکزاده شفارودی, آزاده. سنگ‌‌نگاری، زمین‌شیمی و جایگاه زمین‌ساختی واحدهای آتشفشانی منطقه شاه سلطان علی (جنوب غربی بیرجند). مجله زمین شیمی ایران, 1397; 26(2): 369-382. doi: 10.29252/ijcm.26.2.369

سنگ‌‌نگاری، زمین‌شیمی و جایگاه زمین‌ساختی واحدهای آتشفشانی منطقه شاه سلطان علی (جنوب غربی بیرجند)

مجله بلورشناسی و کانی شناسی ایران
مقاله 9، دوره 26، شماره 2 - شماره پیاپی 72، تیر 1397، صفحه 369-382    اصل مقاله (2.27 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.26.2.369
نویسندگان
سمانه نادرمزرجی؛ محمدحسن کریم‌پور* ؛ آزاده ملکزاده شفارودی
دانشگاه فردوسی مشهد،
چکیده
سنگ‌های آتشفشانی منطقه شاه سلطان علی در جنوب غربی بیرجند و در بخش شرقی پهنه لوت رخنمون دارند. براساس بررسی­های سنگ­نگاری، این سنگ‌ها بازالت تا آندزیت بوده و کانی‌های اصلی آنها پلاژیوکلاز، کلینوپیروکسن، هورنبلند و بندرت بیوتیت و الیوین هستند. آپاتیت و زیرکن به عنوان کانی فرعی در این واحدها شناسایی شده­اند. واحدهای آندزیتی و آندزیت- بازالتی دگرسانی پروپلیتی ضعیف تا متوسط را نشان می­دهند. این واحدها متاآلومین هستند و در گستره سنگ‌هایی با ماهیت آهکی-قلیایی پتاسیم بالا تا شوشونیتی قرار می‌گیرند. برپایه داده‌های زمین­شیمیایی، منطقه مورد بررسی با پهنه فرورانش شرق ایران (پهنه افغان- پهنه لوت) در ارتباط است. اینکه از نظر زمین­ساختی، واحدهای منطقه در کمان قاره‌ای جای می‌گیرند، همچنین غنی‌شدگی از عناصر سنگ دوست بزرگ یون مانند K ,Ba ,Sr و Cs نسبت به عناصر با پتانسیل یونی بالا (Nb - Ti و Zr) همراه با ناهنجاری منفی Nb نشان­دهنده تشکیل ماگما در پهنه فرورانش است. خاستگاه ماگمای تشکیل­دهنده آندزیت و آندزیت- بازالت‌های منطقه، براساس نسبت Ta/Yb, Th/Yb ,Ba/La و Th/Nd گوشته دگرنهاد شده است و سیال‌های حاصل از فرورانش در غنی‌شدگی گوشته نقش بسزایی داشته‌اند. نسبت (La/Yb)N (90/4 تا 59/10) به همراه الگوی عناصر کمیاب نشان­دهنده وجود مقدار جزئی گارنت در خاستگاه است که الگوسازی‌های انجام شده نشان می‌دهد، که ماگمای مولد واحدهای سنگی از ذوب­بخشی 5 تا 20 درصد اسپینل گارنت لرزولیت حاصل شده است.    
کلیدواژه‌ها
پلاژیوکلاز؛ آهکی قلیایی؛ متاآلومین؛ فرورانش؛ پهنه لوت؛ بیرجند
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