ویژگی‌های سیال کانسنگ‌ساز سامانه رگه‌ای طلادار کوارتز، برپایه بررسی میانبارهای سیال، اندریان (شمال غرب ایران)

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه شهید بهشتی

2 دانشگاه صنعتی اصفهان

چکیده

منطقه اندریان در شمال تبریز، شمال غرب ایران واقع بوده و از نظر جایگاه زمین­ساختی بخشی از پهنه ماگمایی اهر- ارسباران است. واحدهای سنگی این منطقه شامل توده نفوذی کم­عمق، رسوبات فلیش­گونه کرتاسه، سنگ­های دگرگونی (هورنفلس و اسکارن) و سنگ­های آتشفشانی هستند. در این منطقه، کانه­زایی به دو صورت اولیه و ثانویه رخ داده است. کانه­زایی درونزاد شامل طلا، پیریت، استیبنیت و کانی­سازی برونزاد شامل مالاکیت، آزوریت و هیدروکسیدهای آهن است. میانبارهای دوفازی غنی از مایع و دوفازی غنی از گاز متداول­ترین میانبارهای سیال در نمونه­های مورد بررسی هستند. رگه­های کوارتز واجد طلا میانگین دمای تشکیل 237 درجه سانتیگراد و شوری پایین (با میانگین 7/8 درصد وزنی معادل نمک طعام) دارند. فشار محاسبه شده برای زمان به تله افتادن میانبارهایی با بالاترین فراوانی بین 26 تا 51 بار برآورد شده که معادل با عمق 270 تا 550 متری است. براساس داده­های دمای همگن­شدگی و شوری، فرآیند کانه­زایی در منطقه اندریان با محیط فراگرمایی مشابهت دارد.      

کلیدواژه‌ها

عنوان مقاله [English]

Characteristics of the ore- bearing quartz veins using fluid inclusions, Andarian, NW Iran

نویسندگان [English]

  • Namnabat 1
  • Ghorbani 1
  • Tabatabaee 2
1 Shahid BeheshtiUniversity
2 Isfahan University of Technology
چکیده [English]

Andarian area is located north of Tabriz city, north west Iran, and tectonically is a part of Ahar-Arasbaran magmatic belt. Geology of the area includes Miocene shallow pluton, Cretaceous flysch-type sediments, metamorphic rocks )hornfels and skarn( and volcanic rocks. Mineralization occurred in two stages: primary and secondary. The primary ore minerals include Au, pyrite and stibnite. Malachite, azurite and iron-hydroxides are the main minerals of the secondary phase. Two phases of liquid-rich and gas-rich inclusions are the most common type of inclusions. The average formation temperature of quartz-gold vein deposit is 237°C with low salinity (with an average of 8.7 wt% NaCl equivalent). The pressure of entrapment for fluid inclusions is between 26 to 51 bars, which is equal to the depth of 270-550 m. Based on fluid inclusions studies, the gold bearing quartz veins formed in epithermal condition.

کلیدواژه‌ها [English]

  • quartz
  • fluid Inclusion
  • gold mineralization
  • Andarian

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  • تاریخ دریافت: 26 آبان 1397
  • تاریخ بازنگری: 07 دی 1397
  • تاریخ پذیرش: 18 بهمن 1397

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