سامانه مدیریت نشریات علمی دانشگاه دامغان

مرادپور, علی, زارعی سهامیه, رضا, احمدی خلجی, احمد, ساریخانی, رامین. (1404). بررسی واکنش گدازه/سنگ، ذوب‌بخشی و خاستگاه پریدوتیت‌های کرمانشاه به کمک شواهد بافتی و شیمی کانی. مجله زمین شیمی ایران, 26(1), 161-178. doi: 10.29252/ijcm.26.1.161
علی مرادپور; رضا زارعی سهامیه; احمد احمدی خلجی; رامین ساریخانی. "بررسی واکنش گدازه/سنگ، ذوب‌بخشی و خاستگاه پریدوتیت‌های کرمانشاه به کمک شواهد بافتی و شیمی کانی". مجله زمین شیمی ایران, 26, 1, 1404, 161-178. doi: 10.29252/ijcm.26.1.161
مرادپور, علی, زارعی سهامیه, رضا, احمدی خلجی, احمد, ساریخانی, رامین. (1404). 'بررسی واکنش گدازه/سنگ، ذوب‌بخشی و خاستگاه پریدوتیت‌های کرمانشاه به کمک شواهد بافتی و شیمی کانی', مجله زمین شیمی ایران, 26(1), pp. 161-178. doi: 10.29252/ijcm.26.1.161
مرادپور, علی, زارعی سهامیه, رضا, احمدی خلجی, احمد, ساریخانی, رامین. بررسی واکنش گدازه/سنگ، ذوب‌بخشی و خاستگاه پریدوتیت‌های کرمانشاه به کمک شواهد بافتی و شیمی کانی. مجله زمین شیمی ایران, 1404; 26(1): 161-178. doi: 10.29252/ijcm.26.1.161

بررسی واکنش گدازه/سنگ، ذوب‌بخشی و خاستگاه پریدوتیت‌های کرمانشاه به کمک شواهد بافتی و شیمی کانی

مجله بلورشناسی و کانی شناسی ایران
مقاله 13، دوره 26، شماره 1 - شماره پیاپی 69، فروردین 1397، صفحه 161-178    اصل مقاله (3.81 M)
شناسه دیجیتال (DOI): 10.29252/ijcm.26.1.161
نویسندگان
علی مرادپور؛ رضا زارعی سهامیه* ؛ احمد احمدی خلجی؛ رامین ساریخانی
دانشگاه لرستان
چکیده
افیولیت کرمانشاه واقع در کمربند افیولیتی بیرونی زاگرس با اجزاء مختلف گوشته­ای و پوسته­ای، بازمانده­ای از شاخه جنوبی اقیانوس نئوتتیس در ایران به شمار می­آید. نمودارهای تقسیم­بندی کانی­ها بیانگر ترکیب فورستریتی الیوین در دونیت، هارزبورژیت و لرزولیت­ها و ترکیب کریزولیتی الیوین در ورلیت­ها و نیز برای ارتوپیروکسن و کلینوپیروکسن­ها به ترتیب نشان دهنده ترکیب انستانیتی و دیوپسید تا اوژیتی هستند. شواهد بافتی چون تیغه­های جدایشی کلینوپیروکسن در ارتوپیروکسن و دانه­های زنجیر مانند اسپینل در کانی­های موجود در سنگ­های فامافیک منطقه­های صحنه، هرسین- نورآباد و میانراهان شواهدی از سرد شدن همراه با کاهش فشار، گدازه­بخشی و واکنش مذاب/سنگ را نشان می­دهند. مودال بسیار پایین کلینوپیروکسن، الیوین غنی از منیزیم و مقدار بالای Cr# و نسبت  Cr/Alدر اسپینل­های مناطق مورد بررسی همگی نشان­دهنده نرخ ذوب­بخشی بالا برای هارزبورژیت و دونیت­ها هستند. مقادیر Al2O3، TiO2 و FeO/MgO محاسبه شده در گدازه مولد اسپینل­­ها و همه نمودارهای تعیین کننده محیط زمین­ساختی­ماگمایی نشان می­دهند که پریدوتیت منطقه­های مورد بررسی از ماگماهای بونینیتی جلوی قوس (مانند پیکریت­ها و تولئیت­های جزایر قوسی) در موقعیت SSZ شکل گرفته­اند.     
کلیدواژه‌ها
پریدوتیت گوشته‌ای؛ بونینیت؛ قوس؛ واکنش گدازه-سنگ؛ افیولیت کرمانشاه
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