سامانه مدیریت نشریات علمی دانشگاه دامغان

صفرپور فیضی, فاطمه, احمدی خلجی, احمد, زارعی‌سهامیه, رضا, کیانی, مسعود, محمدی چغامارانی, زینب. (1404). سنگ‌نگاری و شیمی کانی زئولیت در گدازه‌های بالشی و دایک‌های دیابازی جنوب غرب الشتر (شمال لرستان). مجله زمین شیمی ایران, 29(4), 889-900. doi: 10.52547/ijcm.29.4.889
فاطمه صفرپور فیضی; احمد احمدی خلجی; رضا زارعی‌سهامیه; مسعود کیانی; زینب محمدی چغامارانی. "سنگ‌نگاری و شیمی کانی زئولیت در گدازه‌های بالشی و دایک‌های دیابازی جنوب غرب الشتر (شمال لرستان)". مجله زمین شیمی ایران, 29, 4, 1404, 889-900. doi: 10.52547/ijcm.29.4.889
صفرپور فیضی, فاطمه, احمدی خلجی, احمد, زارعی‌سهامیه, رضا, کیانی, مسعود, محمدی چغامارانی, زینب. (1404). 'سنگ‌نگاری و شیمی کانی زئولیت در گدازه‌های بالشی و دایک‌های دیابازی جنوب غرب الشتر (شمال لرستان)', مجله زمین شیمی ایران, 29(4), pp. 889-900. doi: 10.52547/ijcm.29.4.889
صفرپور فیضی, فاطمه, احمدی خلجی, احمد, زارعی‌سهامیه, رضا, کیانی, مسعود, محمدی چغامارانی, زینب. سنگ‌نگاری و شیمی کانی زئولیت در گدازه‌های بالشی و دایک‌های دیابازی جنوب غرب الشتر (شمال لرستان). مجله زمین شیمی ایران, 1404; 29(4): 889-900. doi: 10.52547/ijcm.29.4.889

سنگ‌نگاری و شیمی کانی زئولیت در گدازه‌های بالشی و دایک‌های دیابازی جنوب غرب الشتر (شمال لرستان)

مجله بلورشناسی و کانی شناسی ایران
مقاله 13، دوره 29، شماره 4 - شماره پیاپی 84، دی 1400، صفحه 889-900    اصل مقاله (4.3 M)
شناسه دیجیتال (DOI): 10.52547/ijcm.29.4.889
نویسندگان
فاطمه صفرپور فیضی1؛ احمد احمدی خلجی* 1؛ رضا زارعی‌سهامیه1؛ مسعود کیانی2؛ زینب محمدی چغامارانی3
1دانشگاه لرستان
2دانشگاه آزاد اسلامی واحد علوم تحقیقات تهران
3دانشگاه تبریز
چکیده
گدازه­های بالشی و دایک­های دیابازی منطقه جنوب غرب الشتر میزبان گونه­های مختلف از زئولیت­ها و کانی­های ثانوی هستند. زئولیت­ها به صورت بادامکی و رگه­ای و از تجزیه کانی­های اولیه تشکیل شده­اند. براساس بررسی­های صحرایی، پراش پرتوی ایکس (XRD) و تجزیه ریزکاو الکترونی، زئولیت­های ناترولیت (فراوان­ترین زئولیت)، مزولیت، اسکولسیت و آنالسیم در گدازه­های بالشی و دایک­های دیابازی منطقه مورد بررسی شناسایی شدند. میانگین نسبت  Si/Al برای ناترولیت، مزولیت، اسکولسیت و آنالسیم به ترتیب 46/1، 49/1، 62/1 و 29/2 محاسبه شد. این زئولیت­ها طی دو مرحله از سیال­های گرمابی دگرگونی در طول شکستگی­ها و در حفره­های سنگ میزبان در دمای کمتر از 250 درجه سانتی­گراد تشکیل شده­اند. بررسی ویژگی­های زمین­شیمیایی سنگ میزبان زئولیت­ها نشان می­دهد که نوع ماگمای تشکیل دهنده آنها آهکی قلیایی تا تولئیتی و محیط زمین­ساختی آنها وابسته به محیط­های درون صفحه­ای و مورب است.      
کلیدواژه‌ها
لرستان؛ الشتر؛ سنگ‌نگاری؛ شیمی‌کانی؛ زئولیت
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