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Mohammadi S S, Chung S, Arab Dohesaran M, Nakhaei M. Thermobarometry, geochemistry and tectonic setting of volcanic rocks in Bijaem area (northwest of Sarbisheh, east of Iran). www.ijcm.ir 2024; 32 (4) :773-794
URL: http://ijcm.ir/article-1-1933-fa.html
URL: http://ijcm.ir/article-1-1933-fa.html
محمدی سیدسعید، چانگ سون لین، عرب دو حصاران مریم، نخعی ملیحه. دما-فشارسنجی، زمین‌شیمی و جایگاه زمین ساختی سنگهای آتشفشانی منطقه بیژائم (شمال غرب سربیشه، شرق ایران). مجله بلورشناسی و کانی شناسی ایران. 1403; 32 (4) :773-794
سیدسعید محمدی*1 
، سون لین چانگ2 ، مریم عرب دو حصاران1 ، ملیحه نخعی3
، سون لین چانگ2 ، مریم عرب دو حصاران1 ، ملیحه نخعی3
1- گروه زمین‌شناسی، دانشکده علوم، دانشگاه بیرجند، بیرجند، ایران
2- انستیتو علوم زمین، آکادمیا سینیکا، تایپه، تایوان
3- گروه مهندسی معدن، دانشکده مهندسی معدن، عمران، شیمی، دانشگاه صنعتی بیرجند، بیرجند، ایران
2- انستیتو علوم زمین، آکادمیا سینیکا، تایپه، تایوان
3- گروه مهندسی معدن، دانشکده مهندسی معدن، عمران، شیمی، دانشگاه صنعتی بیرجند، بیرجند، ایران
چکیده: (504 مشاهده)
پیرامون روستای بیژائم، در ٢٥کیلومتری شمال غرب سربیشه، سنگهای آتشفشانی وابسته به ترشیری با ترکیب آندزیت، تراکی‌داسیت و داسیت همراه سنگهای آذرآواری شامل توف و برش رخنمون دارند. کانی‌‌‌‌های تشکیل دهنده آندزیت شامل پلاژیوکلاز، پیروکسن، آمفیبول، بیوتیت و در داسیتها شامل پلاژیوکلاز، کوارتز، آمفیبول و بیوتیت هستند. بر اساس نتایج تجزیه ریزکاو الکترونی، گستره ترکیبی پلاژیوکلازها در آندزیت بینAb31، An69 تا Ab49، An51 متغیر است و از نوع لابرادوریت هستند. کلینوپیروکسنها ترکیب اوژیت مایل به دیوپسید و ارتوپیروکسنها ترکیب انستاتیت دارند. دمای تشکیل کلینوپیروکسنها و ارتوپیروکسنهای مورد بررسی، به ترتیب حدود 1200 و 1150 درجه سانتیگراد و فشار زمان تبلور آنها، به ترتیب 2 تا 5 کیلوبار و کمتر از 2 کیلوبار تعیین گردید. این سنگ‌ها دارای ماهیت آهکی قلیایی پتاسیم بالا هستند و غنیشدگی از عناصر سنگ دوست درشت یون (LILE)، ناهنجاری منفی Nb، Ti، P، Sr و ناهنجاری منفی ضعیف Eu نشان میدهند که از ویژگیهای گدازههای آهکی قلیایی وابسته به فرورانش است. با بهرهگیری از نمودارهای تفکیک محیط زمینساختی بر اساس عناصر کمیاب، مشخص گردید که سنگهای بررسی شده، وابسته به حاشیه قاره‌ای فعال هستند. بر پایه نسبت Dy/Yb برای سنگهای آندزیتی منطقه بیژائم (91/1-62/1)، خاستگاه گوشتهای آنها، در قلمرو بین اسپینل و گارنت پریدوتیت با درجه ذوب بخشی حدود 7 تا 10 درصد قرار دارد.
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