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مرادپور, علی, احمدی خلجی, احمد, زارعی سهامیه, رضا, ساریخانی, رامین, امامی میبدی, محمدرضا. (1404). زمین دما-فشارسنجی سنگ‌های فرامافیک‌ صحنه، هرسین- نورآباد (شمال شرق کرمانشاه). مجله زمین شیمی ایران, 29(4), 823-836. doi: 10.52547/ijcm.29.4.823
علی مرادپور; احمد احمدی خلجی; رضا زارعی سهامیه; رامین ساریخانی; محمدرضا امامی میبدی. "زمین دما-فشارسنجی سنگ‌های فرامافیک‌ صحنه، هرسین- نورآباد (شمال شرق کرمانشاه)". مجله زمین شیمی ایران, 29, 4, 1404, 823-836. doi: 10.52547/ijcm.29.4.823
مرادپور, علی, احمدی خلجی, احمد, زارعی سهامیه, رضا, ساریخانی, رامین, امامی میبدی, محمدرضا. (1404). 'زمین دما-فشارسنجی سنگ‌های فرامافیک‌ صحنه، هرسین- نورآباد (شمال شرق کرمانشاه)', مجله زمین شیمی ایران, 29(4), pp. 823-836. doi: 10.52547/ijcm.29.4.823
مرادپور, علی, احمدی خلجی, احمد, زارعی سهامیه, رضا, ساریخانی, رامین, امامی میبدی, محمدرضا. زمین دما-فشارسنجی سنگ‌های فرامافیک‌ صحنه، هرسین- نورآباد (شمال شرق کرمانشاه). مجله زمین شیمی ایران, 1404; 29(4): 823-836. doi: 10.52547/ijcm.29.4.823

زمین دما-فشارسنجی سنگ‌های فرامافیک‌ صحنه، هرسین- نورآباد (شمال شرق کرمانشاه)

مجله بلورشناسی و کانی شناسی ایران
مقاله 9، دوره 29، شماره 4 - شماره پیاپی 84، دی 1400، صفحه 823-836    اصل مقاله (3.38 M)
شناسه دیجیتال (DOI): 10.52547/ijcm.29.4.823
نویسندگان
علی مرادپور* 1؛ احمد احمدی خلجی2؛ رضا زارعی سهامیه2؛ رامین ساریخانی2؛ محمدرضا امامی میبدی2
1مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی استان کرمانشاه
2دانشگاه لرستان
چکیده
افیولیت­های صحنه، هرسین – نورآباد (استان کرمانشاه) واقع در کمربند افیولیتی بیرونی زاگرس، بخشی از نوار افیولیتی کرتاسه هستند که به عنوان بازمانده­­های شاخه جنوبی اقیانوس از عمان تا شمال غرب سوریه، قبرس و آنتالیا بر سپر عربی- تائوریک فرا­رانده شده­اند. محاسبه ضریب جدایش نسبت  Fe/Mgبرای کانی الیوین بیانگر خاستگاه گوشته­ای این کانی است. شواهد بافتی موجود در سنگ­های فرامافیک نشان از سرد شدن همزمان با کاهش فشار، ذوب بخشی و واکنش مذاب/سنگ دارند. نمودار­های تعیین کننده محیط زمین­ساختی ماگمایی افزون بر نمایش نمونه­ها در میدان آرایش گوشته­ای الیوین- اسپینل بیانگر قرارگیری آن­ها در میدان پریدوتیت­های منطقه ابر فرورانش (SSZ) است. بر اساس محاسبات انجام شده با واسنجی­های مختلف، دما و فشار تبلور سنگ­های هارزبورژیتی و لرزولیتی 1100 تا 1500 درجه سانتیگراد و 12 تا 18 کیلوبار و برای نمونه ورلیتی 1200 تا 1500 سانتیگراد و 21 تا 23 کیلوبار است که با محیط تشکیل SSZ همخوانی دارد.    
کلیدواژه‌ها
فرامافیک؛ منطقه ابرفرورانش؛ زمین دما- فشار سنجی؛ افیولیت؛ کرمانشاه
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