سامانه مدیریت نشریات علمی دانشگاه دامغان

محمدی نیائی, رامین, نظافتی, نیما, قربانی, منصور, شیخ‌ذکریایی, جمال, دلیران, فرحناز. (1401). کانی‌شناسی و تغییرات شیمیایی سولفوسالت‌های کانسار سرب و روی فراگرمایی آی قلعه‌سی (جنوب‌شرق تکاب، شمال‌غرب ایران). مجله زمین شیمی ایران, 30(2), 223-238. doi: 10.52547/ijcm.30.2.223
رامین محمدی نیائی; نیما نظافتی; منصور قربانی; جمال شیخ‌ذکریایی; فرحناز دلیران. "کانی‌شناسی و تغییرات شیمیایی سولفوسالت‌های کانسار سرب و روی فراگرمایی آی قلعه‌سی (جنوب‌شرق تکاب، شمال‌غرب ایران)". مجله زمین شیمی ایران, 30, 2, 1401, 223-238. doi: 10.52547/ijcm.30.2.223
محمدی نیائی, رامین, نظافتی, نیما, قربانی, منصور, شیخ‌ذکریایی, جمال, دلیران, فرحناز. (1401). 'کانی‌شناسی و تغییرات شیمیایی سولفوسالت‌های کانسار سرب و روی فراگرمایی آی قلعه‌سی (جنوب‌شرق تکاب، شمال‌غرب ایران)', مجله زمین شیمی ایران, 30(2), pp. 223-238. doi: 10.52547/ijcm.30.2.223
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 زمین شیمی ایران, 1401; 30(2): 223-238. doi: 10.52547/ijcm.30.2.223

کانی‌شناسی و تغییرات شیمیایی سولفوسالت‌های کانسار سرب و روی فراگرمایی آی قلعه‌سی (جنوب‌شرق تکاب، شمال‌غرب ایران)

مجله بلورشناسی و کانی شناسی ایران
مقاله 3، دوره 30، شماره 2 - شماره پیاپی 86، تیر 1401، صفحه 223-238    اصل مقاله (5.94 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.52547/ijcm.30.2.223
نویسندگان
رامین محمدی نیائی* 1؛ نیما نظافتی1؛ منصور قربانی2؛ جمال شیخ‌ذکریایی1؛ فرحناز دلیران3
1دانشگاه علوم تحقیقات تهران
2دانشگاه شهید بهشتی تهران
3دانشگاه کارلسروهه آلمان
چکیده
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.       
کلیدواژه‌ها
آی قلعه‌سی؛ فعالیت دوباره گسل‌ها؛ ریزپردازش الکترونی؛ گریزندگی گوگرد و آرسنیک؛ سولفوسالت سری تنانتیت– تتراهدریت
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