دوره 32، شماره 4 - ( 10-1403 )                   جلد 32 شماره 4 صفحات 812-795 | برگشت به فهرست نسخه ها


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Ansari Z, Poosti M, Ghadami G, Fadaeian M. Mineral chemistry, thermobarometry and petrogenesis of ultramafic rocks of Sahraroud, northeast of Bandar Abbas, Iran. www.ijcm.ir 2024; 32 (4) :795-812
URL: http://ijcm.ir/article-1-1929-fa.html
انصاری ذبیح اله، پوستی محمد، قدمی غلامرضا، فدائیان محمد. شیمی کانی، دما-فشار سنجی و سنگ‌زایی سنگ‌های فرامافیک صحرارود، شمال شرق بندرعباس، ایران. مجله بلورشناسی و کانی شناسی ایران. 1403; 32 (4) :795-812

URL: http://ijcm.ir/article-1-1929-fa.html


1- گروه زمین شناسی، دانشگاه هرمزگان، بندرعباس، ایران.
2- گروه زمین شناسی، دانشگاه پیام نور، تهران، ایران.
چکیده:   (255 مشاهده)
منطقه مورد بررسی در شمال شرقی استان هرمزگان واقع است. این منطقه در تقسیم­های ساختاری بین پهنه­های زاگرس و مکران در کمربند افیولیتی کهنوج -رودان - میناب قرار دارد و شامل سنگ‌های فرامافیک چون هارزبورژیت، لرزولیت، ‏دونیت است. کانی­های اصلی این سنگ­ها بیشتر شامل الیوین، ‏ارتوپیروکسن، کلینوپیروکسن، سرپانتینیت، کروم اسپینل هستند. ‏براساس شیمی کانی‌ها، بلورهای الیوین ترکیب کریزولیت- فورستریت (‏Fo85‎‏ تا ‏Fo89‎‏) دارند. ارتوپیروکسن‌ها ترکیب برونزیت- انستاتیت و کلینوپیروکسن­ها ترکیب دیوپسیدی را نشان می‌دهند. کلینوپیروکسن‌ها در دمای بین 1037 تا 1207 و فشار بالا حدود 6 تا 10 کیلوبار متبلور شده­اند. کانی کروم اسپینل بیشتر ترکیب یکنواخت دارد و با غنی‌شدگی از ‏Al2O3‎‏‌ و ‏TiO2‎‏ و ‏ماهیت گوشته‌ای، دارای کمترین مقدار تهی‌شدگی است و تا 14 درصد ذوب­بخشی را نشان می­دهد. ‏سنگ‌های فرامافیک این منطقه در گستره نوع آلپی قرار دارند. ‏پایین بودن مقدار ‏Al2O3‎‏ و بالا بودن مقدار‎ #Mg ‎در ارتوپیروکسن‌ها و ترکیب فورستریتی (‏Fo85‎‏ تا ‏Fo89‎‏) الیوین‌ها با ‏مقدار پایین ‏CaO‏ در آنها نشان می­دهد که ذوب­بخشی مهم‌ترین رخداد در تشکیل سنگ‌های ‏فرامافیک‌ این منطقه است و شکل‌گیری این سنگ‌ها از نظر زمین­ساختی با محیط ‏فرورانشی مورب سازگار است.‏
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نوع مقاله: پژوهشي | موضوع مقاله: تخصصي

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