سامانه مدیریت نشریات علمی دانشگاه دامغان

پارسایی, محمد, درگاهی, سارا, آروین, محسن, شاکر, علیرضا, نظافتی, نیما. (1401). سنگ‌نگاری، زمین‌شیمی و سنگ‌زایی سنگ‌های گرانیتوئیدی درآلو، جنوب کرمان. مجله زمین شیمی ایران, 30(2), 311-326. doi: 10.52547/ijcm.30.2.311
محمد پارسایی; سارا درگاهی; محسن آروین; علیرضا شاکر; نیما نظافتی. "سنگ‌نگاری، زمین‌شیمی و سنگ‌زایی سنگ‌های گرانیتوئیدی درآلو، جنوب کرمان". مجله زمین شیمی ایران, 30, 2, 1401, 311-326. doi: 10.52547/ijcm.30.2.311
پارسایی, محمد, درگاهی, سارا, آروین, محسن, شاکر, علیرضا, نظافتی, نیما. (1401). 'سنگ‌نگاری، زمین‌شیمی و سنگ‌زایی سنگ‌های گرانیتوئیدی درآلو، جنوب کرمان', مجله زمین شیمی ایران, 30(2), pp. 311-326. doi: 10.52547/ijcm.30.2.311
پارسایی, محمد, درگاهی, سارا, آروین, محسن, شاکر, علیرضا, نظافتی, نیما. سنگ‌نگاری، زمین‌شیمی و سنگ‌زایی سنگ‌های گرانیتوئیدی درآلو، جنوب کرمان. مجله زمین شیمی ایران, 1401; 30(2): 311-326. doi: 10.52547/ijcm.30.2.311

سنگ‌نگاری، زمین‌شیمی و سنگ‌زایی سنگ‌های گرانیتوئیدی درآلو، جنوب کرمان

مجله بلورشناسی و کانی شناسی ایران
مقاله 9، دوره 30، شماره 2 - شماره پیاپی 86، تیر 1401، صفحه 311-326    اصل مقاله (2.08 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.52547/ijcm.30.2.311
نویسندگان
محمد پارسایی1؛ سارا درگاهی* 2؛ محسن آروین2؛ علیرضا شاکر3؛ نیما نظافتی1
1دانشگاه آزاد اسلامی واحد علوم و تحقیقات
2دانشگاه شهید باهنر کرمان
3مجتمع آموزش عالی زرند
چکیده
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.     
کلیدواژه‌ها
سنگ‌های گرانیتی؛ نوع I؛ فرورانش؛ کمان ماگمایی ارومیه – دختر؛ کرمان
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