دما-فشارسنجی، زمین‌شیمی و جایگاه زمین ساختی سنگ‌های آتشفشانی منطقه بیژائم (شمال غرب سربیشه، شرق ایران)

نوع مقاله : مقاله پژوهشی

نویسندگان

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

چکیده

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 < /span>، 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.

کلیدواژه‌ها

عنوان مقاله [English]

Thermobarometry, geochemistry and tectonic setting of volcanic rocks in Bijaem area (northwest of Sarbisheh, east of Iran)

نویسندگان [English]

  • Seyyed Saeid Mohammadi 1
  • Sun-Lin Chung 2
  • Maryam Arab Dohesaran 1
  • Malihe Nakhaei 3
1 Department of geology, Faculty of Sciences, University of Birjand, Birjand, Iran
2 Institute of earth sciences, Academia Sinica, Taipei, Taiwan
3 Department of Mining Engineering, Faculty of Civil, Mining and Chemistry, Birjand University of Technology, Birjand, Iran
چکیده [English]

Around Bijaem village about 25 Km northwest of Sarbisheh, Tertiary volcanic rocks include of andesite, trachydacite and dacite with pyroclastic deposits such as tuff and breccia are cropped out. The forming minerals of andesite are plagioclase, pyroxene, hornblende and biotite and the dacites are composed of plagioclase, quartz, hornblende and biotite. Based on microprobe analyses, the composition of plagioclases in andesite variable from Ab31 An69 to Ab49An51 and are labradorite type. Clinopyroxenes are augite inclined to diopside and orthopyroxene have enstatite composition. The crystallization temperature of studied clinopyroxene and orthopyroxenes  are 1200°C and1150°C respectively and pressure at their crystallization time was 2-5 kb and <2 kb respectively. These rocks have high-K calc alkaline nature and show enrichment of LILE and negative anomaly of Nb, Ti, P, Sr  and weak europium anomaly that indicate subduction related calk alkaline lavas. Using discriminant diagrams. based on trace elements, the studied rocks belong to active continental margin. Dy/Yb ratio for Bijaem area andesitic rocks (1.62-1.91) show that their mantle source located at field between spinel and garnet peridotite with 7-10 percent partial melting degree.

کلیدواژه‌ها [English]

  • Andesite
  • Thermobarometry
  • spinel iherzolite
  • Bijaem
  • active continental margin
  • Lut block

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  • تاریخ دریافت: 24 اردیبهشت 1403
  • تاریخ بازنگری: 17 خرداد 1403
  • تاریخ پذیرش: 06 تیر 1403

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