سنگ نگاری و شیمی کانی انواع مختلف سنگ‌های متاسوماتیتی در ارتباط با کانی‌زایی آهن- آپاتیت نوع کایرونا در منطقه بافق، با تمرکز بر کانسارهای چغارت و چادرملو، ایران مرکزی

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه شهید بهشتی

2 دانشگاه تهران

چکیده

کانسارهای آهن- آپاتیت چغارت و چادرملو در کرانه غربی قطعه بافق قرار دارند و پی­سنگ دگرگونی پرکامبرین به سن نئوپروتروزوییک پسین، واحدهای رسوبی- آتشفشانی پرکامبرین پسین و توده­های نفوذی پرکامبرین پسین- کامبرین پیشین میزبان آنها در منطقه بافق هستند. خاستگاه و ارتباط سنگ­هایی که از دیرباز با نام متاسوماتیت شناخته می­شوند، همواره با پرسش همراه بوده است. براساس بررسی­های سنگ­نگاری و شیمی کانی انجام شده، پنج نوع دگرسانی گرمابی در این سنگ­ها تشخیص داده شده است. قدیمی­ترین آن­ها، دگرسانی سدیمی بوده که در فواصل دورتر از ذخایر آهن رخ داده است و با حضور کانی آلبیت با بافت شطرنجی شناخته می­شود. دگرسانی جوانتر سدیمی-کلسیمی، یک مدل دگرنهادی بزرگ و دو مرحله­ای است که با حضور ترمولیت- اکتینولیت مشخص می­­شود و همزمان با کانی­سازی آهن رخ داده است. دگرسانی پتاسیمی بعدی، در اثر هجوم مایع­های غنی از پتاسیم و تشکیل فلدسپار پتاسیم و بیوتیت ثانویه بوجود آمده است. دگرسانی­های سیلیسی و سریسیتی بطور تاْخیری در منطقه رخ داده­اند.     

کلیدواژه‌ها

عنوان مقاله [English]

Petrography and mineral chemistry of metasomatites related to Iron-Apatite mineralization in Kiruna-type deposits in the Bafq region with a focus on Choghart and Chadormalu mining district, Central Iran

نویسندگان [English]

  • Somayeh Teimouri 1
  • Mansour Ghorbani 1
  • Soroush Modabberi 2
1
2
چکیده [English]

The Iron-apatite deposits of Choghart and Chadormalu mining district are located in the western margin of the Bafq block and are hosted by Precambrian metamorphic basement complex, Late Precambrian sedimentary-volcanic units, and Late Precambrian-Early Cambrian plutonic rocks. The origin and relation of the rocks for a long time, which are known as metasomatites, have always been questioned. Based on petrography and mineral chemistry studies, five types of hydrothermal alterations have identified in these rocks. The oldest one is Na-alteration, which occurs at farther distances of iron deposits and is characterized by the presence of chessboard albite. The youngerst one is sodic-calcic alteration which is widespread and two-stages of the metasomatism model are characterized by the presence of tremolite-actinolite and is synchronous with the Fe-oxides. Potassic alteration occurs after two previous alteration phases, because of the influence of K-rich fluids and the formation of K-feldspar and secondary biotite. Silicate and sericite alteration has occurred as a late phase in the region.
 

کلیدواژه‌ها [English]

  • Iron-apatite deposits
  • Bafq mining district
  • Chadormalu deposits
  • Choghart deposits
  • Kiruna
  • metasomatism
  • Mineral chemistry

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  • تاریخ دریافت: 23 بهمن 1400
  • تاریخ بازنگری: 27 اردیبهشت 1401
  • تاریخ پذیرش: 18 خرداد 1401

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