سامانه مدیریت نشریات علمی دانشگاه دامغان

قلی‌پور, میثم, براتی, مهرداد, طالع‌فاضل, ابراهیم, هورای, وراتیسلاو. (1399). روابط ‌بافتی- شیمیایی کانی‌های آپاتیت- مونازیت- زنوتیم در کانسار آهن± آپاتیت لکه‌سیاه (شمال‌شرق بافق): شواهدی از تکوین یک سامانه گرمابی. مجله زمین شیمی ایران, 28(1), 51-70. doi: 10.29252/ijcm.28.1.51
میثم قلی‌پور; مهرداد براتی; ابراهیم طالع‌فاضل; وراتیسلاو هورای. "روابط ‌بافتی- شیمیایی کانی‌های آپاتیت- مونازیت- زنوتیم در کانسار آهن± آپاتیت لکه‌سیاه (شمال‌شرق بافق): شواهدی از تکوین یک سامانه گرمابی". مجله زمین شیمی ایران, 28, 1, 1399, 51-70. doi: 10.29252/ijcm.28.1.51
قلی‌پور, میثم, براتی, مهرداد, طالع‌فاضل, ابراهیم, هورای, وراتیسلاو. (1399). 'روابط ‌بافتی- شیمیایی کانی‌های آپاتیت- مونازیت- زنوتیم در کانسار آهن± آپاتیت لکه‌سیاه (شمال‌شرق بافق): شواهدی از تکوین یک سامانه گرمابی', مجله زمین شیمی ایران, 28(1), pp. 51-70. doi: 10.29252/ijcm.28.1.51
قلی‌پور, میثم, براتی, مهرداد, طالع‌فاضل, ابراهیم, هورای, وراتیسلاو. روابط ‌بافتی- شیمیایی کانی‌های آپاتیت- مونازیت- زنوتیم در کانسار آهن± آپاتیت لکه‌سیاه (شمال‌شرق بافق): شواهدی از تکوین یک سامانه گرمابی. مجله زمین شیمی ایران, 1399; 28(1): 51-70. doi: 10.29252/ijcm.28.1.51

روابط ‌بافتی- شیمیایی کانی‌های آپاتیت- مونازیت- زنوتیم در کانسار آهن± آپاتیت لکه‌سیاه (شمال‌شرق بافق): شواهدی از تکوین یک سامانه گرمابی

مجله بلورشناسی و کانی شناسی ایران
مقاله 4، دوره 28، شماره 1 - شماره پیاپی 77، فروردین 1399، صفحه 51-70    اصل مقاله (3.53 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.28.1.51
نویسندگان
میثم قلی‌پور1؛ مهرداد براتی* 1؛ ابراهیم طالع‌فاضل1؛ وراتیسلاو هورای2
1دانشگاه بوعلی‌سینا
2موسسه علوم زمین اسلواکی
چکیده
کانسار آهن± آپاتیت لکه­سیاه در ایالت فلززایی بافق- ساغند (ایران مرکزی) و در سنگ­های میزبان ریولیتی قرار گرفته است. کانی­های اصلی در این کانسار مگنتیت و آپاتیت هستند که کانی­های مونازیت و زنوتیم به صورت میانبار درون بلور و شکستگی­های این دو کانی تشکیل شده­اند. کانی­ها با استفاده از روش­های میکروسکوپی و تجزیه ریزکاوالکترونی بررسی شدند. نتایج نشان می­دهد که بلور آپاتیت اولیه بوده و احتمالاً از ماگمای نخستین با ماهیت مافیک تا فرامافیک نهشته شده است. بلورهای آپاتیت دارای منطقه­بندی نامنظم از فازهای تیره و روشن هستند، به­طوری که بخش­های تیره آپاتیت غنی از میانبارهای مونازیت و زنوتیم ثانویه است. این نتایج با فرآیند انحلال- ته­نشینی مجدد سازگار است. طی این فرآیند، بلورهای آپاتیت با سیال­های گرمابی تأخیری که در راستای مرزهای بلوری در حال مهاجرت بوده­اند واکنش داده­ و تهی از عناصر خاکی نادر (REE) شده­اند. همچنین عناصر خاکی نادر دستخوش جدایش ترجیحی شده­اند، به طوری که اغلب عناصر خاکی نادر سبک (LREE) در مونازیت و عناصر نادر سنگین (HREE) در زنوتیم غنی شده­اند.    
کلیدواژه‌ها
کانسارهای اکسید آهن±آپاتیت؛ کانی‌های عناصر خاکی نادر؛ دگرنهادی؛ فرآیند انحلال- ته‌نشینی مجدد
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