سامانه مدیریت نشریات علمی دانشگاه دامغان

غارسی, مهدی, رسا, ایرج, یزدی, محمد. (1404). بررسی کانی سازی اسکارن مزرعه، شمال اهر، با تاکید بر مطالعه میانبارهای شاری. مجله زمین شیمی ایران, 26(1), 229-244. doi: 10.29252/ijcm.26.1.229
مهدی غارسی; ایرج رسا; محمد یزدی. "بررسی کانی سازی اسکارن مزرعه، شمال اهر، با تاکید بر مطالعه میانبارهای شاری". مجله زمین شیمی ایران, 26, 1, 1404, 229-244. doi: 10.29252/ijcm.26.1.229
غارسی, مهدی, رسا, ایرج, یزدی, محمد. (1404). 'بررسی کانی سازی اسکارن مزرعه، شمال اهر، با تاکید بر مطالعه میانبارهای شاری', مجله زمین شیمی ایران, 26(1), pp. 229-244. doi: 10.29252/ijcm.26.1.229
غارسی, مهدی, رسا, ایرج, یزدی, محمد. بررسی کانی سازی اسکارن مزرعه، شمال اهر، با تاکید بر مطالعه میانبارهای شاری. مجله زمین شیمی ایران, 1404; 26(1): 229-244. doi: 10.29252/ijcm.26.1.229

بررسی کانی سازی اسکارن مزرعه، شمال اهر، با تاکید بر مطالعه میانبارهای شاری

مجله بلورشناسی و کانی شناسی ایران
مقاله 18، دوره 26، شماره 1 - شماره پیاپی 69، فروردین 1397، صفحه 229-244    اصل مقاله (6.22 M)
شناسه دیجیتال (DOI): 10.29252/ijcm.26.1.229
نویسندگان
مهدی غارسی* ؛ ایرج رسا؛ محمد یزدی
دانشگاه شهید بهشتی
چکیده
کانسار اسکارن مزرعه در کمربند فلززایی قفقاز کوچک – البرز غربی بر اثر تزریق توده گرانیتوییدی شیورداغ به سن اولیگومیوسن به درون مجموعه کربناته، آتشفشانی قدیمی­تر و به شکل برون اسکارن گارنت ـ اپیدوت­دار ایجاد شده است. ترکیب کانی­شناسی فلزی شامل مگنتیت، پیریت، کالکوپیریت، بورنیت، کوولیت، هماتیت، گوتیت و مالاکیت است و بیشتر کانه­زایی در مرحله اسکارن پسرونده ایجاد شده است. نتایج تجزیه عناصر فرعی نشانگر تاثیر شاره­های با خاستگاه پوسته بر توده نفوذی طی فرآیندهای اسکارن­زایی است. در کانی­های کوارتز و کلسیت نمونه­های اسکارن دو دسته شاره درگیر نوع (L+V) با شوری کم تا متوسط (57/1 تا 94/17درصد وزنی نمک) و گستره دمای همگن­شدگی 120 تا 356 درجه و نوع (L+V+S)  با شوری زیاد (06/32 تا 77/41 درصد وزنی نمک) و گستره دمای همگن­شدگی 227 تا 375 درجه سانتی­گراد دیده می­شوند که هر دو در مرحله اسکارن پسرونده ایجاد شده­اند. خاستگاه میانبارهای شاره­ای نوع(L+V)  و نوع (L+V+S) به ترتیب شاره­های دگرگونی و ترکیب ماگمایی – شورابه­های سطحی هستند. دو فرآیند آمیختگی هم­دمای شاره­های با شوری مختلف و رقیق­شدگی سطحی شاره­ها بر اثر مخلوط شدن آب­های جوی با شاره­های ماگمایی- دگرگونی عوامل اصلی تکوین شاره­های کانه­ساز هستند. فشار شاره در زمان تشکیل کانسنگ در حدود 100 بار و دمای تقریبی بین 250 تا 340 درجه سانتی­گراد بوده است و بر این اساس می­توان کانسار اسکارن مزرعه را با ژرفای تشکیل 350 تا 400 متر نسبت به سطح ایستابی قدیمی، به عنوان یک کانسار اسکارن کم ژرفا معرفی کرد.    
کلیدواژه‌ها
کمربند فلززایی قفقاز کوچک - البرز غربی؛ کانسار مزرعه؛ اسکارن؛ میانبارهای شاری؛ ریزدماسنجی
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