سنگ‌شناسی، زمین‌شیمی و شیمی‌کانی سنگ‌های آتشفشانی شمال کبودرآهنگ (همدان)

نوع مقاله : مقاله پژوهشی

نویسندگان

دانشگاه لرستان

چکیده

سنگ­های آتشفشانی شمال کبودرآهنگ با ترکیب آندزیت و تراکی آندزیت به سن ائوسن در پهنه ارومیه-دختر بصورت ستون­های منشوری عمودی رخنمون یافته­اند. این سنگ­ها دارای درشت بلورهایی از آمفیبول و پلاژیوکلاز با بافت پورفیری، گلومروپورفیری و ریزسنگی هستند. شواهد زمین شیمیایی نشان می­دهد که این سنگ­ها از سری ماگمایی آهکی قلیایی هستند و از نظر محیط زمین­ساختی در کرانه­های فعال قاره­ای وابسته به قوس تشکیل شده­اند که می­تواند با فروررانش اقیانوس نئوتتیس به زیر ایران مرکزی مربوط باشد. همچنین، الگوی عناصر خاکی نادر و نمودارهای عنکبوتی بهنجار شده، غنی­شدگی از عناصر خاکی نادر سبک (LREE) و عناصر سنگ دوست بزرگ یون (LILE) در مقایسه با عناصر با شدت میدان بالا (HFSE) و عناصر خاکی نادر سنگین (HREE) را نشان می­دهند که از شواهد محیط­های فرورانشی است. بر اساس نتایج به دست آمده از شیمی کانی آمفیبول­ها مشخص شد که این کانی­ها در گستره­ی آمفیبول­های کلسیمی و از نوع منیزیوهورنبلند تا چرماکیت بوده و وابسته به کرانه­های فعال قاره­ای هستند که با نتایج سنگ میزبان همخوانی دارد. براساس محاسبات دما فشارسنجی، این آمفیبول­ها در دمای تعادلی 5/815 درجه سانتیگراد و فشار 35/6 کیلوبار تشکیل شده­اند. گریزندگی بالای به دست آمده برای این سنگ­ها نشان دهنده شرایط اکسایشی در پیدایش این سنگ­ها و گواهی بر پیدایش آنها در مرز صفحه­های همگراست.

کلیدواژه‌ها

عنوان مقاله [English]

Petrology, geochemistry and minearal chemistry of volcanic rocks in the north of Kaboudarahang (Hamedan)

نویسندگان [English]

  • Nazari
  • Tahmasbi
  • Ahmadi Khalaji
چکیده [English]

The volcanic rocks in the north of Kaboudarahang consist of andesite-tracky andesite with the Eocene age have been exposed in the Uromieh-Dokhtar zone. These andesite are scattered as prasmatic columns. Petrographic studies show that these rocks consist of amphibole and plagioclase with porphyritic, glomoroporphyritic and microlitic tetures. Geochemical studies show that these rocks belong to the calc alkaline magmatic series. In terms of tectonic environment, they are located in the active continental margin associated with subduction zone. Trace element patern shows the enrichment of LREE to HREE. Amphibole mineral chemistry shows that they are belonging to the calcic group of magnesium hornblend and chermackit types. These amphiboles belong to active continental margin that consistent with the results of host andesite. Based on thermobarometric methods, these amphiboles are formed at a temperature of 815.5 ° C and a pressure of 6.35 kbar. The high fugacity obtained for these rocks indicates the oxidant conditions in the formation of these rocks and evidence of their formation at the boundary of convergent plates.

کلیدواژه‌ها [English]

  • Thermobarometry
  • Andesite
  • Eocene
  • volcanic arc
  • Kaboudarahang

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  • تاریخ دریافت: 24 بهمن 1398
  • تاریخ بازنگری: 03 فروردین 1399
  • تاریخ پذیرش: 06 اردیبهشت 1399

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