فصلنامه علمی علوم زمین

فصلنامه علمی علوم زمین

ویژگی‌های دگرسانی و کانه‌زایی کانسار مس دهنه‌گمرکان: شواهدی از یک سامانه پورفیری احیایی در کمان ماگمایی ارومیه- دختر

نوع مقاله : مقاله پژوهشی

نویسندگان
1 گروه زمین‌شناسی اقتصادی، دانشکده علوم پایه، دانشگاه تربیت مدرس، تهران، ایران
2 شرکت صنایع معدنی فرآوری مس امید سبزواران، تهران، ایران
10.22071/gsj.2026.570993.2242
چکیده
کانسار مس دهنه‌گمرکان، که در بخش جنوبی کمربند پورفیری کرمان در کمان ماگمایی ارومیه- دختر واقع است، یکی از معدود سامانه‌هایی است که شواهدی از شکل‌گیری در یک محیط ماگمایی- گرمابی با ماهیت احیایی نشان می‌دهد. بررسی‌های میدانی، سنگ‌نگاری، دگرسانی و کانه‌زایی در این پژوهش با اتکا بر داده‌های حاصل از رخنمون‌های صحرایی، گمانه‌های حفاری، مقاطع نازک و صیقلی و تحلیل‌های کانی‌شناسی (XRD)، ویژگی‌های زمین‌شیمیایی و کانه‌زایی این سامانه را معرفی می‌نماید. در این کانسار 3 مرحله از توده‌­های نفوذی جایگیر شده با سن پس از ائوسن با ترکیب‌های گرانودیوریت، تونالیت و کوارتزمونزونیت تا کوارتزمونزودیوریت شناسایی شده‌اند که توده کوارتزمونزونیت تا کوارتز مونزودیوریت میزبان اصلی کانی‌سازی مس است. پهنه‌های دگرسانی شامل سیلیسی، پتاسیک، فیلیک، آرژیلیک، پروپیلیتیک و کربناتی هستند. رخداد گسترده دگرسانی پتاسیک همراه با کانی‌های سولفیدی ژرف‌زاد (هیپوژن)، نبود مگنتیت، هماتیت ژرف‌زاد و انیدریت و رخداد کانی‌های احیایی مانند پیروتیت، ایلمنیت و آرسنوپیریت، همگی نشان‌دهنده ماهیت کاهنده سامانه است. الگوهای دگرسانی، ویژگی‌های کانی‌سازی و رابطه آن‌ها با توده‌های نفوذی، شواهد ارزشمندی از تشکیل این کانسار در یک محیط احیایی فراهم آورده است که در مقایسه با مدل‌های کلاسیک پورفیری اکسیدان در ایران، ویژگی‌های کانی‌شناسی و فلززایی متفاوتی دارد. این نتایج نه‌تنها الگویی جدید برای تفسیر فرایندهای دگرسانی و کانه‌زایی در جنوب کمربند کرمان ارائه می‌کند، بلکه می‌تواند در بازنگری مدل‌های اکتشافی و شناسایی سایر سامانه‌های پورفیری احیایی در کمان ماگمایی ارومیه- دختر نقشی کلیدی ایفا کند.
کلیدواژه‌ها
موضوعات

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دوره 36، شماره 3 - شماره پیاپی 141
پاییز 1405، سال سی‌ و ششم، شماره 3، پیاپی 141
پاییز 1405
صفحه 79-102