سامانه مدیریت نشریات علمی دانشگاه دامغان

تیموری, سیده سمیه, قربانی, منصور, مدبری, سروش. (1404). سنگ نگاری و شیمی کانی انواع مختلف سنگ‌های متاسوماتیتی در ارتباط با کانی‌زایی آهن- آپاتیت نوع کایرونا در منطقه بافق، با تمرکز بر کانسارهای چغارت و چادرملو، ایران مرکزی. مجله زمین شیمی ایران, 30(4), 667-682. doi: 10.52547/ijcm.30.4.667
سیده سمیه تیموری; منصور قربانی; سروش مدبری. "سنگ نگاری و شیمی کانی انواع مختلف سنگ‌های متاسوماتیتی در ارتباط با کانی‌زایی آهن- آپاتیت نوع کایرونا در منطقه بافق، با تمرکز بر کانسارهای چغارت و چادرملو، ایران مرکزی". مجله زمین شیمی ایران, 30, 4, 1404, 667-682. doi: 10.52547/ijcm.30.4.667
تیموری, سیده سمیه, قربانی, منصور, مدبری, سروش. (1404). 'سنگ نگاری و شیمی کانی انواع مختلف سنگ‌های متاسوماتیتی در ارتباط با کانی‌زایی آهن- آپاتیت نوع کایرونا در منطقه بافق، با تمرکز بر کانسارهای چغارت و چادرملو، ایران مرکزی', مجله زمین شیمی ایران, 30(4), pp. 667-682. doi: 10.52547/ijcm.30.4.667
تیموری, سیده سمیه, قربانی, منصور, مدبری, سروش. سنگ نگاری و شیمی کانی انواع مختلف سنگ‌های متاسوماتیتی در ارتباط با کانی‌زایی آهن- آپاتیت نوع کایرونا در منطقه بافق، با تمرکز بر کانسارهای چغارت و چادرملو، ایران مرکزی. مجله زمین شیمی ایران, 1404; 30(4): 667-682. doi: 10.52547/ijcm.30.4.667

سنگ نگاری و شیمی کانی انواع مختلف سنگ‌های متاسوماتیتی در ارتباط با کانی‌زایی آهن- آپاتیت نوع کایرونا در منطقه بافق، با تمرکز بر کانسارهای چغارت و چادرملو، ایران مرکزی

مجله بلورشناسی و کانی شناسی ایران
مقاله 7، دوره 30، شماره 4 - شماره پیاپی 90، دی 1401، صفحه 667-682    اصل مقاله (4.64 M)
شناسه دیجیتال (DOI): 10.52547/ijcm.30.4.667
نویسندگان
سیده سمیه تیموری* 1؛ منصور قربانی1؛ سروش مدبری2
1دانشگاه شهید بهشتی
2دانشگاه تهران
چکیده
کانسارهای آهن- آپاتیت چغارت و چادرملو در کرانه غربی قطعه بافق قرار دارند و پی­سنگ دگرگونی پرکامبرین به سن نئوپروتروزوییک پسین، واحدهای رسوبی- آتشفشانی پرکامبرین پسین و توده­های نفوذی پرکامبرین پسین- کامبرین پیشین میزبان آنها در منطقه بافق هستند. خاستگاه و ارتباط سنگ­هایی که از دیرباز با نام متاسوماتیت شناخته می­شوند، همواره با پرسش همراه بوده است. براساس بررسی­های سنگ­نگاری و شیمی کانی انجام شده، پنج نوع دگرسانی گرمابی در این سنگ­ها تشخیص داده شده است. قدیمی­ترین آن­ها، دگرسانی سدیمی بوده که در فواصل دورتر از ذخایر آهن رخ داده است و با حضور کانی آلبیت با بافت شطرنجی شناخته می­شود. دگرسانی جوانتر سدیمی-کلسیمی، یک مدل دگرنهادی بزرگ و دو مرحله­ای است که با حضور ترمولیت- اکتینولیت مشخص می­­شود و همزمان با کانی­سازی آهن رخ داده است. دگرسانی پتاسیمی بعدی، در اثر هجوم مایع­های غنی از پتاسیم و تشکیل فلدسپار پتاسیم و بیوتیت ثانویه بوجود آمده است. دگرسانی­های سیلیسی و سریسیتی بطور تاْخیری در منطقه رخ داده­اند.     
کلیدواژه‌ها
کانسار آهن- آپاتیت؛ منطقه معدنی بافق؛ کانسار چادرملو؛ کانسار چغارت؛ کایرونا؛ دگرنهادی؛ شیمی کانی
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