دوره 27، شماره 2 - ( 4-1398 )                   جلد 27 شماره 2 صفحات 281-294 | برگشت به فهرست نسخه ها

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Moradi R, Boomeri M, Bagheri S. Mineral chemistry of apatite in the Lar igneous complex, North of Zahedan. www.ijcm.ir. 2019; 27 (2) :281-294
URL: http://ijcm.ir/article-1-1265-fa.html
مرادی راحله، بومری محمد، باقری ساسان. بررسی شیمی آپاتیت در مجموعه آذرین لار، شمال زاهدان. مجله بلورشناسی و کانی شناسی ایران. 1398; 27 (2) :281-294

URL: http://ijcm.ir/article-1-1265-fa.html

دانشگاه سیستان و بلوچستان
چکیده:   (34 مشاهده)
مجموعه آذرین لار در پهنه جوش خورده سیستان واقع است. سنگ‌های آذرین به شکل استوک، دایک، گدازه و آذرآواری هستند. کانی‌زایی مس- مولیبدن به وسیله سیال­های گرمابی در استوک‌ها تشکیل شده است. آپاتیت فراوان‌ترین کانی فرعی در سنگ‌های آذرین مورد بررسی است که به شکل­های منشوری و برشی قابل مشاهده است. بر پایه نتایج ریزکاوالکترونی، آپاتیت‌های مورد بررسی از نوع فلوئور آپاتیت و با مقدار کمی کلر هستند که نشان دهنده تعادل آن با یک مذاب/ سیال نسبتاً آبدار و اکسایشی است. این مذاب/ سیال در گستره سامانه‌های کانی‌زایی شده دنیا قرار می‌گیرد. حضور آپاتیت‌های کلر پایین و سنگ‌های میزبان پتاسیم بالا (شوشونیتی) می‌تواند نشان دهنده جدایش کلر - پتاسیم ماگمای اولیه باشد که نیازمند آبزدایی رسوبات فرورانده شده در گوشته سنگ کره­ای عمیق و همچنین رخداد تبلور جدایشی در سنگ‌های لار است.    
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نوع مطالعه: پژوهشي | موضوع مقاله: تخصصي
دریافت: ۱۳۹۸/۳/۱۲ | پذیرش: ۱۳۹۸/۳/۱۲ | انتشار: ۱۳۹۸/۳/۱۲

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