دوره 30، شماره 2 - ( 3-1401 )
جلد 30 شماره 2 صفحات 326-311 |
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Parsaei, Dargahi, Arvin, Shaker, Nezafati. Petrography, geochemistry and petrogenesis of the Daraloo granitoid rocks, south of Kerman. www.ijcm.ir 2022; 30 (2) :311-326
URL: http://ijcm.ir/article-1-1756-fa.html
URL: http://ijcm.ir/article-1-1756-fa.html
پارسایی محمد، درگاهی سارا، آروین محسن، شاکر علیرضا، نظافتی نیما. سنگ‌نگاری، زمین‌شیمی و سنگ‌زایی سنگهای گرانیتوئیدی درآلو، جنوب کرمان. مجله بلورشناسی و کانی شناسی ایران. 1401; 30 (2) :311-326
محمد پارسایی1 
، سارا درگاهی* 2، محسن آروین2 ، علیرضا شاکر3 ، نیما نظافتی1
، سارا درگاهی* 2، محسن آروین2 ، علیرضا شاکر3 ، نیما نظافتی1
1- دانشگاه آزاد اسلامی واحد علوم و تحقیقات
2- دانشگاه شهید باهنر کرمان
3- مجتمع آموزش عالی زرند
2- دانشگاه شهید باهنر کرمان
3- مجتمع آموزش عالی زرند
چکیده: (1271 مشاهده)
گستره کانسار درآلو از نظر ساختاری در پهنه ایران مرکزی و کمان ماگمایی ارومیه دختر و در جنوب استان کرمان واقع است. در این منطقه، روانههای آندزیتی و سنگهای آذرآواری ائوسن در معرض تودههای نفوذی نیمه عمیق الیگومیوسن قرار گرفتهاند. اغلب نمونههای نفوذی از نوع گرانودیوریت پورفیری تا مونزوگرانیت پورفیری با زمینه ریزدانهای هستند و دگرسانی شدید از نوع فیلیک نشان میدهند. براساس شواهد کانیشناسی و زمین شیمیایی، سنگهای گرانیتوئیدی درآلو در سری آهکی قلیایی جای میگیرند و دارای طبیعت متاآلومین تا کمی پرآلومین و از نوع I هستند. در بیشتر نمونهها، ناهنجاری منفی آشکاری از Nb-Ti دیده میشود که این امر با جدایش فازهای تیتانیومدار چون تیتانیت و تیتانومگنتیت توجیه میشود. همچنین غنیشدگی آشکار در عناصر سنگ دوست درشت یون (چون K، Rb، Ba و Cs) و عناصر خاکی نادر سبک نسبت به عناصر با شدت میدان بالا (چون، Nb، Ti و Zr) و عناصر خاکی نادر سنگین، از ویژگیهای زمین شیمیایی ماگماهای تولید شده در محیطهای فرورانش هستند. بنابراین چنین برداشت میشود که سنگهای گرانیتی درآلو باید در یک محیط کرانه فعال قارهای، به علت فرورانش پوسته اقیانوسی نئوتتیس به زیر ایران مرکزی در زمان ترشیری به وجود آمده باشند.
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