سامانه مدیریت نشریات علمی دانشگاه دامغان

نخعی, ملیحه, محمدی, سید سعید. (1404). زمین‌شناسی، ویژگی‌های فیزیکی، کانی‌شناسی و زمین‌شیمی بنتونیت اشکفتوک (شمال غرب بیرجند). مجله زمین شیمی ایران, 29(4), 871-888. doi: 10.52547/ijcm.29.4.871
ملیحه نخعی; سید سعید محمدی. "زمین‌شناسی، ویژگی‌های فیزیکی، کانی‌شناسی و زمین‌شیمی بنتونیت اشکفتوک (شمال غرب بیرجند)". مجله زمین شیمی ایران, 29, 4, 1404, 871-888. doi: 10.52547/ijcm.29.4.871
نخعی, ملیحه, محمدی, سید سعید. (1404). 'زمین‌شناسی، ویژگی‌های فیزیکی، کانی‌شناسی و زمین‌شیمی بنتونیت اشکفتوک (شمال غرب بیرجند)', مجله زمین شیمی ایران, 29(4), pp. 871-888. doi: 10.52547/ijcm.29.4.871
نخعی, ملیحه, محمدی, سید سعید. زمین‌شناسی، ویژگی‌های فیزیکی، کانی‌شناسی و زمین‌شیمی بنتونیت اشکفتوک (شمال غرب بیرجند). مجله زمین شیمی ایران, 1404; 29(4): 871-888. doi: 10.52547/ijcm.29.4.871

زمین‌شناسی، ویژگی‌های فیزیکی، کانی‌شناسی و زمین‌شیمی بنتونیت اشکفتوک (شمال غرب بیرجند)

مجله بلورشناسی و کانی شناسی ایران
مقاله 12، دوره 29، شماره 4 - شماره پیاپی 84، دی 1400، صفحه 871-888    اصل مقاله (5.32 M)
شناسه دیجیتال (DOI): 10.52547/ijcm.29.4.871
نویسندگان
ملیحه نخعی* 1؛ سید سعید محمدی2
1دانشگاه صنعتی بیرجند
2دانشگاه بیرجند
چکیده
 معدن بنتونیت اشکفتوک در شمال غرب بیرجند و در بخش شرقی قطعه لوت قرار دارد. این بنتونیت فراورده دگرسانی گدازه­های آندزیتی و توف­های همراه به سن ترشیری است. ویژگی­های زمین­شیمیایی نشان می­دهند که سنگ مادر بنتونیت­ها دارای ترکیب آندزیتی و نمونه­های بنتونیت دارای ترکیب آندزیت تا داسیت- ریوداسیت هستند. سری ماگمایی  همه نمونه­های بررسی­شده از نوع آهکی­قلیایی است. بر اساس نتایج پراش پرتوی ایکس (XRD)، کانی­های اصلی سازنده بنتونیت­ها شامل مونتموریونیت، آنورتیت، کریستوبالیت و کوارتز همراه با مقادیر کمتر ایلیت، مسکوویت، کائولینیت، میکروکلین و دولومیت هستند. تصاویر میکروسکوپ الکترونی تهیه­ شده از نمونه­های بنتونیت نشان می­دهد که اسمکتیت (مونتموریونیت) فراوان­ترین کانی در این نمونه­هاست که با ریخت­­شناسی ورقه­ای با لبه­های ناهموار، لانه­زنبوری و دانه­ذرتی مشخص می­شود. بر پایه نتایج طیف­سنجی پراکنش انرژی پرتوی ایکس (EDX) نیز کانی غالب سازنده بنتونیت­ها از نوع مونتموریونیت سدیم –کلسیم­دار است و بر این اساس، بنتونیت اشکفتوک در رده بنتونیت­های نوع وایومینگ قرار دارد. بررسی تغییرات جرم عناصر اصلی و کمیاب بنتونیت­های اشکفتوک بیانگر کاهیدگی اجزایی چونK2O، Na2O، CaO، MgO، MnO و عناصر سنگ­دوست بزرگ­یون مانند Ba، Rb، Sr و غنی­شدگی اجزایی چون SiO2، Al2O3 و Fe2O3 است.       
کلیدواژه‌ها
مونتموریونیت؛ تغییر جرم؛ اشکفتوک؛ لوت
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