سامانه مدیریت نشریات علمی دانشگاه دامغان

غدیرپور, مرضیه, ترابی, قدرت, قادری, مرجان, بیات, فرشته, شیردشت زاده, نرگس. (1402). فرایند‌های ماگمایی در ارتباط با تشکیل سنگ‌‌های آتشفشانی آندزیتی ائوسن کوه کلوت قندهاری (شمال غرب انارک، استان اصفهان). مجله زمین شیمی ایران, 31(3), 497-508. doi: 10.61186/ijcm.31.3.497
مرضیه غدیرپور; قدرت ترابی; مرجان قادری; فرشته بیات; نرگس شیردشت زاده. "فرایند‌های ماگمایی در ارتباط با تشکیل سنگ‌‌های آتشفشانی آندزیتی ائوسن کوه کلوت قندهاری (شمال غرب انارک، استان اصفهان)". مجله زمین شیمی ایران, 31, 3, 1402, 497-508. doi: 10.61186/ijcm.31.3.497
غدیرپور, مرضیه, ترابی, قدرت, قادری, مرجان, بیات, فرشته, شیردشت زاده, نرگس. (1402). 'فرایند‌های ماگمایی در ارتباط با تشکیل سنگ‌‌های آتشفشانی آندزیتی ائوسن کوه کلوت قندهاری (شمال غرب انارک، استان اصفهان)', مجله زمین شیمی ایران, 31(3), pp. 497-508. doi: 10.61186/ijcm.31.3.497
غدیرپور, مرضیه, ترابی, قدرت, قادری, مرجان, بیات, فرشته, شیردشت زاده, نرگس. فرایند‌های ماگمایی در ارتباط با تشکیل سنگ‌‌های آتشفشانی آندزیتی ائوسن کوه کلوت قندهاری (شمال غرب انارک، استان اصفهان). مجله زمین شیمی ایران, 1402; 31(3): 497-508. doi: 10.61186/ijcm.31.3.497

فرایند‌های ماگمایی در ارتباط با تشکیل سنگ‌‌های آتشفشانی آندزیتی ائوسن کوه کلوت قندهاری (شمال غرب انارک، استان اصفهان)

مجله بلورشناسی و کانی شناسی ایران
مقاله 6، دوره 31، شماره 3 - شماره پیاپی 91، مهر 1402، صفحه 497-508    اصل مقاله (4.55 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.61186/ijcm.31.3.497
نویسندگان
مرضیه غدیرپور1؛ قدرت ترابی* 1؛ مرجان قادری1؛ فرشته بیات1؛ نرگس شیردشت زاده2
1گروه زمین‌شناسی، دانشگاه اصفهان، اصفهان، ایران
2بخش زمین شناسی، دانشکده علوم پایه، دانشگاه تربیت مدرس، تهران، ایران
چکیده
کوه کلوت قندهاری در حدود 40 کیلومتری شمال غرب انارک (استان اصفهان) واقع است. این منطقه بخشی از ایران مرکزی است و در غرب قطعه یزد و نزدیک به افیولیت عشین و محل عبور گسل کویر بزرگ قرار دارد. در شمال غرب انارک، مجموعه افیولیتی عشین، با سنگ آهک‏‌های پالئوسن پوشانده شده و با سنگ‏‌های آتشفشانی ائوسن قطع گردیده است. سنگ‏‌های آتشفشانی ائوسن نیز با استوک گابرویی-دیوریتی ائوسن پسین قطع شده‏‌اند. سنگ‌های آتشفشانی ائوسن کوه کلوت قندهاری بیشتر از نوع آندزیت بوده که در نمونه دستی از خاکستری تیره تا روشن متغیر بوده و دارای بیگانه­سنگ‌های آمفیبولیت هستند. بافت‏‌های پورفیری، خال خال، جریانی، غربالی و گلومروپورفیری مهم‌ترین بافت‌ها هستند. درشت‌بلورهای سازنده این آندزیت‏‌ها شامل پلاژیوکلاز، آمفیبول و کلینوپیروکسن هستند و زمینه سنگ نیز از این کانی‌ها و نیز سانیدین، مگنتیت و آپاتیت تشکیل شده است. کانی‏‌های زئولیت،کلریت، اپیدوت، سریسیت، کائولینیت و کلسیت نیز کانی های ثانویه ناشی از دگرسانی هستند. نتایج تجزیه شیمی کانی‏‌ها نشان می‌دهد که پلاژیوکلازها از نوع آندزین تا لابرادوریت (مقدار آنورتیت 1/30 تا 3/52 درصد)، پتاسیم فلدسپارها از نوع سانیدین (مقدار ارتوکلاز 6/68 تا 3/71 درصد)، آمفیبول‏‌ها کلسیمی و از نوع پارگاسیت (با عدد منیزیم 58/0 تا 71/0) و کلینوپیروکسن‏‌ها از نوع دیوپسید (با عدد منیزیم 91/0 تا 93/0) هستند. داده‌های زمین شیمیایی سنگ کل عناصر اصلی نشان می‌دهد که این سنگ‌ها بیشتر از نوع آندزیت و تراکی‌آندزیت‌های آهکی قلیایی هستند. درنمودارهای سنگ‏‌های آتشفشانی ائوسن کوه کلوت قندهاری بهنجار شده نسبت به کندریت و گوشته اولیه، نمونه ها غنی از عناصر خاکی نادر سبک (LREE) و عناصر سنگ دوست بزرگ یون (LILE) و فقیر از عناصر با شدت میدان بالا (HFSE؛ چون (Ti, Ta, Nb هستند که مشخصه‏‌ای از فعالیت ماگمایی در ارتباط با فرورانش است. داده‏‌های زمین­شیمیایی نشان می‌دهند که ماگمای اولیه سازنده سنگ‌های آتشفشانی ائوسن این منطقه از ذوب­بخشی با درجه متوسط یک اسپینل لرزولیت گوشته سنگ کره ای به‌دست آمده­اند. دلیل رخداد این فعالیت آتشفشانی نیز به احتمال بسیار فرورانش پوسته اقیانوسی نئوتتیس پیرامون خردقاره شرق- ایران مرکزی (پوسته اقیانوسی عشین و نایین) است. این سنگ‌ها از نظر محیط زمین­ساختی شبیه سنگ‌های موجود در قوس‌های آتشفشانی هستند.       
کلیدواژه‌ها
سنگ‌های آتشفشانی ائوسن؛ آندزیت؛ آهکی قلیایی؛ کوه کلوت قندهاری؛ انارک؛ ایران مرکزی
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