دمافشارسنجی توده‌های نفوذی غرب تفت بر پایه داده‌های شیمی کانی‌ها

نوع مقاله : مقاله پژوهشی

نویسنده

گروه زمین‌شناسی، دانشگاه پیام نور، تهران، ایران

چکیده

بررسی توده‌های گرانیتوئیدی غرب تفت، در بخش میانی پهنه ایران مرکزی، بیانگر حضور کانی‌های کوارتز، ارتوکلاز، پلاژیوکلاز به عنوان کانی‌های اصلی و آمفیبول، بیوتیت، اسفن، زیرکن و آپاتیت به عنوان کانی‌های فرعی است. در این سنگ­ها، بافت‌های دانه­ای دانه‌متوسط تا دانه‌ریز، گرانوفیری و میرمیکیتی دیده می‌شوند. داده‌های تجزیه شیمی کانی‌‎ها نشان می‌دهد که در این توده‎ها، آمفیبول‎های نوع کلسیمی با ماهیت منیزیوهورنبلند تا اکتینولیت در دمای oC 891-659، فشار Kbar 1/2-9/4 و عمق Km 4/4-6 متبلور شده‌اند. همچنین فلدسپارهای نوع الیگوکلاز تا آندزین متعلق به دمای oC 700-800، و بیوتیت‌های نوع منیزیم‌دار متعلق به دمای C° 700-750 متبلور شده‌اند. شیمی کانی بیوتیت نشانگر ماهیت گوشته‌ای ماگمای سازنده این سنگ‌هاست که طی صعود دچار آلایش پوسته‌ای متوسط تا شدید شده‌اند. شیمی کانی کلریت به دخالت فرآیندهای دگرسانی و تشکیل این کانی در دمای 330 تا 360 درجه سانتی‌گراد اشاره دارد. ترکیب همه داده‌ها گویای ماهیت آهکی قلیایی نوع I توده‌های نفوذی مورد بررسی است که در پهنه ساختاری فرورانش و در ارتباط با کرانه قاره‌ای فعال تشکیل شده‌اند.

کلیدواژه‌ها

عنوان مقاله [English]

Thermobarometry of intrusive masses in west of Taft using mineral chemistry data

نویسنده [English]

  • Javad Ghanei Ardakani
Department of Geology, Payame Noor University, Tehran, Iran
چکیده [English]

The study of granitoides bodeis in the west of Taft, is located in the middle part of the central Iran, indicates the presence of quartz, orthoclase, plagioclase minerals as main minerals and amphibole, biotite, sphene, zircon and apatite as secondary minerals. In these rocks, medium-grained to fine-grained, granophyric and myrmikite textures are observed. The data of mineral chemistry analysis show that calcic type amphiboles of magnesiohornblende to actinolite nature belonging to temperature 659-891 C, pressure 2.1- 4.9, and depth 4.4- 6 have been crystallized. However, feldspars are oligoclase to andesine type that belonging to 700-800 C, and biotites have been crystallized 700-750 C. The minerals chemistry of biotite was indicated to the mantle nature of the magma, which has suffered from moderate to severe crustal contamination during ascent. The mineral chemistry of chlorite refers to the involvement of alteration processes and the formation of this mineral at the temperature of 330 to 360 C. All of the data indicates to the calc-alkaline granitoides I type, which were formed in the structural zone of subduction and in connection with the active continental margin

کلیدواژه‌ها [English]

  • Mineral chemistry
  • granitoid bodies
  • calc-alkaline
  • westTaft
  • barometery

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  • تاریخ دریافت: 27 دی 1402
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