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رجائیه, مریم, مرتضوی, سید محسن, قلمقاش, جلیل, عمرانی, جعفر. (1397). کلریت‌زایی بیوتیت در گنبدهای داسیتی باغات (جنوب سیرجان). مجله زمین شیمی ایران, 26(2), 399-408. doi: 10.29252/ijcm.26.2.399
مریم رجائیه; سید محسن مرتضوی; جلیل قلمقاش; جعفر عمرانی. "کلریت‌زایی بیوتیت در گنبدهای داسیتی باغات (جنوب سیرجان)". مجله زمین شیمی ایران, 26, 2, 1397, 399-408. doi: 10.29252/ijcm.26.2.399
رجائیه, مریم, مرتضوی, سید محسن, قلمقاش, جلیل, عمرانی, جعفر. (1397). 'کلریت‌زایی بیوتیت در گنبدهای داسیتی باغات (جنوب سیرجان)', مجله زمین شیمی ایران, 26(2), pp. 399-408. doi: 10.29252/ijcm.26.2.399
رجائیه, مریم, مرتضوی, سید محسن, قلمقاش, جلیل, عمرانی, جعفر. کلریت‌زایی بیوتیت در گنبدهای داسیتی باغات (جنوب سیرجان). مجله زمین شیمی ایران, 1397; 26(2): 399-408. doi: 10.29252/ijcm.26.2.399

کلریت‌زایی بیوتیت در گنبدهای داسیتی باغات (جنوب سیرجان)

مجله بلورشناسی و کانی شناسی ایران
مقاله 11، دوره 26، شماره 2 - شماره پیاپی 72، تیر 1397، صفحه 399-408    اصل مقاله (2.29 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.26.2.399
نویسندگان
مریم رجائیه* 1؛ سید محسن مرتضوی1؛ جلیل قلمقاش2؛ جعفر عمرانی2
1دانشگاه هرمزگان
2سازمان زمین شناسی و اکتشافات معدنی کشور
چکیده
گنبدهای داسیتی منطقه باغات در جنوب سیرجان و پهنه سنندج-سیرجان قرار دارند. کانی­های اصلی تشکیل­دهنده این سنگ­ها شامل پلاژیوکلاز و کلینوپیروکسن و کانی­های فرعی شامل بیوتیت، زیرکن و آپاتیت است. ترکیب شیمیایی بیوتیت­ها در این سنگ­ها نشان می­دهد که این کانی­ها به کانی­های کلریت و احتمالاً همرشدی­هایی با کانی روتیل دگرسان شده­اند. مقدار Fe/(Fe+Mg) در گستره 53/0 تا 57/0 و مقدار Si در گستره 7/5 تا 15/6 بوده و معرف کانی پیکنوکلریت است. در این کلریت­ها مقدار جزء کلریت (Xc)، بین 43/0 تا 85/0 قرار دارد که اشاره به وجود لایه­های اسمکتیت در ساختار کلریت دارد. ترکیب شیمیایی کلریت دمای تشکیل این کانی را 252 تا 263 درجه سانتیگراد نشان می­دهد و بیانگر ماهیت آهکی-قلیایی ماگمای سازنده سنگ­های مورد بررسی است که در مناطق کوهزایی تشکیل شده است.
کلیدواژه‌ها
شیمی کانی؛ کلریت؛ بیوتیت؛ باغات؛ پهنه سنندج-سیرجان
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آمار
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