بررسی تاثیر الگوی ساختاری منطقه شمال شرق ایران بر مدل کانی زایی آهن در آنومالی C شمالی سنگ آهن سنگان

نویسندگان

1 دانشجوی دکتری، گروه مهندسی معدن، دانشکده مهندسی معدن و متالورژی، دانشگاه صنعتی امیرکبیر، تهران

2 دانشیار، گروه مهندسی معدن، دانشکده مهندسی معدن و متالورژی، دانشگاه صنعتی امیرکبیر، تهران

3 استادیار، سازمان زمین‌شناسی و اکتشافات معدنی ایران

چکیده

سیستم‌های ساختاری مرتبط با کانی‌سازی آهن در محدوده ذخایر معدنی سنگان واقع در شمال‌شرق ایران، رابطه مستقیمی با هندسه تغییر شکل‌ها، شکستگی‌ها و گسل‌ها، سایر ساخت‌های صفحه‌ای و خطی و نفوذ توده‌های آذرین به عنوان منشا و منبع حرکت سیالات نهایی ماگماتیسم موثر در کانی‌سازی دارد. هدف از این مطالعه، بررسی و شناسایی ساختارهای تکتونیکی در ذخیره C شمالی سنگان و تحلیل آن‌ها، تعیین مدل ساختار ناحیه‌ای، مدل الگوی ساختاری ذخیره و در نهایت ارایه مدل تشکیل آن ذخیره است. با توجه به قرارگیری منطقه معدنی سنگان در انتهای یکی از پایانه‌های انشعابی بزرگ مقیاس از گسل درونه، این بلوک از لحاظ زمین‌ساخت    ناحیه‌ای، به عنوان بخشی از فرار تکتونیکی مطرح است و می‌توان بسیاری از عملکردهای ساختاری در ناحیه معدنی سنگان را ناشی از فعالیت این پدیده دانست. با بررسی گسل‌های موجود در محدوده ذخیره و انجام تحلیل تراکم فضایی هر سری گسل، نقشه چگالی گسل تهیه شده که نشانگر سه سیستم گسلی در ذخیره C شمالی است. بر اساس مطالعات توده‌های نفوذی، مدل شماتیک که نشان‌دهنده نوع تحرک احتمالی، مکانیزم ساختمان بیرونی و خروج سیالات ماگمایی در هنگام جانشینی ماگما است، به همراه مدل تشکیل ذخیره C شمالی ارایه شد. تشکیل ذخیره C شمالی مرتبط با ساختار است که پایه‌ای برای کاربرد روش تکتونوژئوشیمیایی است. نتایج مطالعه اسکارن‌ها و توده معدنی در ذخایر سنگان (به ویژه C شمالی)، اهمیت زیادی دارد و می‌تواند به صورت محلی برای مطالعه ذخایر اسکارن دیگر که در کنتاکت سنگ‌های کربناته با نفوذی‌های گرانیتی در این نوار معدنی‌اند، مورد استفاده قرار گیرد.

کلیدواژه‌ها

موضوعات

عنوان مقاله [English]

Investigation of Effect of Structural Pattern on Mineralization Model in the C- North Ore Deposit, Sangan, NE Iran

نویسندگان [English]

  • A. Rezaei 1
  • H. Hassani 2
  • P. Moarefvand 2
  • A. Golmohammadi 3
1 Ph.D Student, Dept. of Mining and Metallurgy Engineering, Amirkabir University of Technology, Tehran, Iran
2 Associate Professor, Dept. of Mining and Metallurgy Engineering, Amirkabir University of Technology, Tehran, Iran
3 Assistant Professor, Geological Survey and Mineral Exploration of Iran, Tehran, Iran
چکیده [English]

Structural systems related to iron ore mineralization in the Sangan mining region, northeastern Iran, have a direct relationship with the geometry of deformations. Fractures and faults, linear and planar structures and the influence of igneous bodies as the source of the fluids have the final effect of magmatism on mineralization. The purpose of this study was to investigate and identify the tectonic structures in C-North ore deposit, including a regional structural model with a structural model of ore deposit, and deposit formation model. Due to the location of the Sangan mining area at the end of one of the large-scale branching terminals of the Dorouneh fault, Sangan region is considered as part of the tectonic escape, and many structural functions in the area can be found in the Sangan ore deposits is due to the activity of this phenomenon. By investigating the existing faults in the area and performing a spatial density analysis for each fault series, a fault density map is generated which indicates the three fault systems in the C-North ore deposit. Based on intrusive body studies, the schematic diagram showing the probable accretion style, mechanism of outward building and exsolution of magmatic fluids during the emplacement of magma was presented along with the C-North ore deposit formation model. The results of studying of skarns and C-North ore deposits have great applied scientific significance and can be used for the study of skarn deposits.

کلیدواژه‌ها [English]

  • Structural model
  • Mineralization
  • Tectonic escape
  • C-North deposit
  • Sangan

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سابقه مقاله

  • تاریخ دریافت: 12 دی 1397
  • تاریخ بازنگری: 07 اسفند 1397
  • تاریخ پذیرش: 16 اردیبهشت 1398

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