دوره 30، شماره 2 - ( 3-1401 )                   جلد 30 شماره 2 صفحات 238-223 | برگشت به فهرست نسخه ها


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Mohmmadi Niaei, Nezafati, Ghorbani, Sheikhzakariaei, daliran. Mineralogy and chemical variations of Sulfosalts of epithermal deposit of Ay-Qalasi (southeast of Takab, northwest of Iran). www.ijcm.ir 2022; 30 (2) :223-238
URL: http://ijcm.ir/article-1-1744-fa.html
محمدی نیائی رامین، نظافتی نیما، قربانی منصور، شیخ‌ذکریایی جمال، دلیران فرحناز. کانی‌شناسی و تغییرات شیمیایی سولفوسالت‌های کانسار سرب و روی فراگرمایی آی قلعه‌سی (جنوب‌شرق تکاب، شمال‌غرب ایران). مجله بلورشناسی و کانی شناسی ایران. 1401; 30 (2) :223-238

URL: http://ijcm.ir/article-1-1744-fa.html


1- دانشگاه علوم تحقیقات تهران
2- دانشگاه شهید بهشتی تهران
3- دانشگاه کارلسروهه آلمان
چکیده:   (940 مشاهده)
کانسار فراگرمایی سرب و روی (نقره) آی قلعه‌سی در شمال‌غرب ایران و جنوب‌شرق تکاب واقع است. جایگاه ساختاری آن در برخوردگاه کمربند آتشفشانی ارومیه- دختر با پهنه سنندج- سیرجان است. براساس بررسی­های میکروسکوپی و تجزیه به روش ریزپردازش‌ الکترونی، ترکیب این سولفوسالت‌ها از سری تنانتیت- تتراهدریت است. این کانی‌ها بیشتر در کانی‌های میزبان جایگزین شده­اند و نتایج ریزپردازش الکترونی نشان می­دهد که ترکیب شیمیایی آنها وابسته به ترکیب کانی­شناسی کانه­های سولفیدی میزبان است. با نفوذ گنبدهای داسیتی نزدیک کانسار، سیال­های گرمابی با گریزندگی بالای گوگرد و آرسنیک و به‌طور فرعی آنتیموان تشکیل می‌شوند. فعالیت دوباره گسل­ها سبب برشی شدن کانه­های سولفیدی اولیه شده و زمینه را برای نفوذ سیال­های گرمابی فراهم می­کند. نفوذ و چرخش این سیال­ها در بخش­های برشی شده کانسار به‌دلیل گریزندگی بالای گوگرد و آرسنیک، شرایط ترمودینامیکی جدیدی را برای سامانه موجب شده که خود سبب ناپایداری کانی‌های سولفیدی می‌شود. در وضعیت جدید، خرده­های برشی کانه­های اسفالریت، کالکوپیریت و پیریت با این سیال­ها واکنش کرده و کانه­های سولفوسالت سری تنانتیت- تتراهدریت را بوجود می‌آورند.       
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نوع مقاله: پژوهشي | موضوع مقاله: تخصصي

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