کانی‌شناسی، دگرسانی، زمین‌شیمی و بررسی سیال‌های درگیرکانی‌سازی اکسیدآهن- مس منطقه نامق، شمال شرقی کاشمر

نوع مقاله : مقاله پژوهشی

نویسندگان

دانشگاه فردوسی مشهد

چکیده

منطقه نامق در شمال شرق کاشمر، استان خراسان رضوی، و در مرکز کمربند ماگمایی خواف-کاشمر- بردسکن واقع است. زمین­شناسی منطقه پوشیده از تراکی­آندزیت و واحد­های آذرآواری شامل توف تراکی­آندزیتی تا ریولیتی است که دایک­های مونزودیوریتی در آنها نفوذ کرده­اند. کانی­سازی به شکل رگه­ای با امتداد شمال شرقی- جنوب غربی و شیب 75 درجه به سمت شمال شرقی، در پهنه­های گسلی و در سنگ میزبان تراکی­آندزیت و توف تراکی­آندزیتی تشکیل شده است. کانی­های اولیه شامل اسپکیولاریت، کالکوپیریت و مگنتیت همراه با باطله کوارتز و کانی­های ثانویه شامل گوتیت، هماتیت و مالاکیت است. سیلیسی شدن مهمترین دگرسانی همراه با کانی­سازی است. ناهنجاری قابل ملاحظه مس تا بیش از دو درصد و مقادیر پایین طلا تا 20 میلی­گرم در تن در رگه دیده می­شود. بر پایه بررسی سیال­های درگیر، دمای تشکیل کانی­سازی بین 300 تا 496 درجه سانتیگراد بوده و از محلولی شامل نمک­های NaCl و CaCl2 با درجه شوری 11 تا 22 درصد وزنی بوجود آمده است. آمیختگی دو سیال با دما- شوری بالا و دما- شوری پایین، باعث کاهش دما و شوری و رقیق­شدگی شده و شرایط را برای ته­نشست اکسیدآهن و مس از کمپلکس­های کلریدی فراهم کرده ­است. مدل آمیختگی آب ماگمایی و آب جوی بهترین مدل برای تشکیل رگه­ آهن- مس­دار منطقه نامق است. این کانی­سازی در فشار 10 تا 60 مگاپاسکال و در عمقی بین 5/0 تا 2 کیلومتر (برپایه فشار سنگ­کره) تشکیل شده است. کنارزایی کانیایی، سنگ میزبان، دگرسانی، کنترل ساختاری و ماهیت محلول کانه­دار نشان می­دهد که کانی­سازی از نوع گرمابی مس غنی از اکسید آهن (اکسید آهن-مس) است.

کلیدواژه‌ها

عنوان مقاله [English]

Mineralogy, Alteration, geochemistry, and fluid inclusion studies of Fe oxide-copper mineralization of Namegh area, NE Kashmar

نویسندگان [English]

  • hakimeh Taghadosi
  • azadeh Malekzadeh Shafaroudi
Ferdowsi University of Mashhad
چکیده [English]

Namegh area is located northeast Kashmar, Khorasan Razavi Province, and contral parts of the Khaf-Kashmar-Bardaskan magmatic belt. Geology of the area consists of trachyandesite and pyroclastic rocks including trachyandesitic to rhyolitic tuff, which are intruded by monzodioritic dykes. Mineralization is occurred as vein type with NW-SE trending and 75°NE inclination hosted by trachyandesite and trachyandesitic tuff. Primary minerals are specularite, chalcopyrite, and magnetite and secondary minerals are goethite, hematite, and malachite. Silicification is the most important alteration. High anomaly of Cu (up to 2%) and low values of Au (maximum 20 ppb) are present in the vein. Based on fluid inclusion studies, formation temperature of mineralization is between 300 to 496 ºC and it is occurred from NaCl- and CaCl2-bearing fluid with 11 to 22 wt. % NaCl equivalent salinity. Temperature and salinity is decreased and dilution occurs due to mixing of two high temperature-salinity and low temperature-salinity fluids resulting Fe oxide and copper is deposited from chloride ligands. Mixing of magmatic and meteoric waters model is the best model for generation of Namegh iron-copper vein. This mineralization is occurred at 10 to 60 Mpa pressure and 0.5 to 2 Km depth (assuming lithostatic pressure). Mineral paragenesis, host rock, alteration, structural control, and nature of ore fluid indicate mineralization is Iron oxide-copper hydrothermal type. 

کلیدواژه‌ها [English]

  • Mineralization
  • alteration
  • Geochemistry
  • fluid Inclusion
  • Fe oxide- copper
  • Namegh
  • NE Iran

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  • تاریخ دریافت: 21 تیر 1396
  • تاریخ بازنگری: 16 مهر 1396
  • تاریخ پذیرش: 04 آبان 1396

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