تحلیل بافتی انباشت گویچه‌ای (اسفرولیتی) کانی‌‌ها در سنگ‌های دیوریتی بوئین-میاندشت، پهنه سنندج-سیرجان

نوع مقاله : مقاله پژوهشی

نویسندگان

دانشکده منابع طبیعی و علوم زمین، دانشگاه شهرکرد، شهرکرد، ایران

چکیده

مجموعه بوئین - میاندشت در بخش مرکزی پهنه سنندج - سیرجان، از سنگ‌های دگرگونی و توده‌های گرانیتوئیدی، گابرو و گابرو-دیوریت تشکیل شده است. بررسی­های سنگ­نگاری بر سنگ­های دیوریتی منطقه نشان­­دهنده­ی ­کانی­های اصلی پلاژیوکلاز، آمفیبول و بیوتیت به همراه کانی‌های فرعی کوارتز، آپاتیت، زیرکن و اسـفن است. بافت‌های بین دانه­ای، و آپلیتی به همراه بافت گویچه­ای (شعاعی، رشته­ای) دیده می­شوند. گوی سنگ­ها (اسفرولیت­ها) به صورت مجموعه­ای شعاعی و یا شاخه شعاعی هم­مرکز دیده می­شوند. اندازه گوی­سنگ­ها به طور متوسط تا 2/0 میلی­متر می­رسد و از نظر ریختاری، با شکل­های مختلفی از جمله بادبزنی، تنوره و کروی دیده می­شوند. وجود بافت گویچه­ای در این سنگ‌ها بیانگر شرایط ناپایدار و نامتعادل و همچنین سردشدگی سریع در هنگام تبلور ماگماست. طی برخاست منطقه و در پی آن فرآیند ذوب­شدگی همراه با دگرشکلی و آمیختگی ماگماهای مافیک با ماگمای فلسی بافت گویچه­ای در این سنگ­های نیمه عمیق ایجاد شده است.

کلیدواژه‌ها

عنوان مقاله [English]

Textural analysis of spherulite accumulation of minerals in the Boein-Miandasht dioritic rocks, Sanandaj-Sirjan Zone

نویسندگان [English]

  • Farzaneh Alikhani
  • Nahid Shabanian
  • Alireza Davoudian
Department of Natural Engineering, Faculty of Earth Sciences and Natural Resources, Shahrekord University, Shahrekord, Iran
چکیده [English]

The Boein-Miandasht Complex, in the central part of the Sanandaj-Sirjan Zone, is composed of metamorphic rocks, and granitoid intrusions, gabbro and gabbro-diorite. The mineralogy of diorite includes plagioclase, amphibole, biotite, quartz, apatite, zircon, and titanite. Intergranular and spherulitic (radial and fibrous) textures along with aplitic texture are seen in these rocks. Spherulites are visible as a radial set or a concentric radial branch. The dimensions of the spherulites are on average up to 0.2 mm with different shapes such as fan, plume and spherical in morphology. Spherulite texture is attributed to unstable and unbalanced conditions and rapid cooling during magma crystallization. During the exhumation of the region and the melting along with the deformation and the occurrence of fracturing associated with the mixing of mafic magma with felsic magma, the spherulite texture was created in these hypabyssal rocks.

کلیدواژه‌ها [English]

  • Spherulite
  • Boein-Miandasht Complex
  • Sanandaj-Sirjan Zone
  • diorite

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  • تاریخ دریافت: 03 تیر 1403
  • تاریخ بازنگری: 25 تیر 1403
  • تاریخ پذیرش: 03 مرداد 1403

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