سامانه مدیریت نشریات علمی دانشگاه دامغان

قانعی اردکانی, جواد. (1403). شیمی کانی توده گرانیتوئیدی غرب اردکان (ایران مرکزی). مجله زمین شیمی ایران, 32(2), 325-338. doi: 10.61186/ijcm.32.2.325
جواد قانعی اردکانی. "شیمی کانی توده گرانیتوئیدی غرب اردکان (ایران مرکزی)". مجله زمین شیمی ایران, 32, 2, 1403, 325-338. doi: 10.61186/ijcm.32.2.325
قانعی اردکانی, جواد. (1403). 'شیمی کانی توده گرانیتوئیدی غرب اردکان (ایران مرکزی)', مجله زمین شیمی ایران, 32(2), pp. 325-338. doi: 10.61186/ijcm.32.2.325
قانعی اردکانی, جواد. شیمی کانی توده گرانیتوئیدی غرب اردکان (ایران مرکزی). مجله زمین شیمی ایران, 1403; 32(2): 325-338. doi: 10.61186/ijcm.32.2.325

شیمی کانی توده گرانیتوئیدی غرب اردکان (ایران مرکزی)

مجله بلورشناسی و کانی شناسی ایران
مقاله 10، دوره 32، شماره 2 - شماره پیاپی 94، مرداد 1403، صفحه 325-338    اصل مقاله (1.63 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.61186/ijcm.32.2.325
نویسنده
جواد قانعی اردکانی*
گروه زمین‌شناسی، دانشگاه پیام نور، تهران، ایران
چکیده
توده گرانیتوئیدی غرب اردکان با مجموعه کانی‌های اصلی کوارتز، ارتوکلاز، پلاژیوکلاز و کانی‌های فرعی آمفیبول، بیوتیت، اسفن، زیرکن و آپاتیت در بخش میانی پهنه ایران مرکزی رخنمون دارد. بافت غالب در این توده دانه­ای متوسط تا ریز، گرانوفیری و میرمیکیتی است. بر اساس داده‌های شیمی کانی‌، آمفیبول‌های کلسیمی با ماهیت منیزیوهورنبلند تا اکتینولیت در دمای oC 890-530  متبلور شده‌اند. همزمان، کانی پلاژیوکلاز نوع الیگوکلاز تا آندزین در oC 700-800 و بیوتیت‌های منیزیم‌دار در دمای oC 730-650 متبلورشده‌اند. همچنین با توجه به شرایط اکسایشی، کانی‌های کدر نوع مگنتیت تشکیل شده‌اند. داده­های شیمی همه این کانی‌ها به ماهیت گوشته‌ای ماگمای سازنده آنها اشاره دارد، که طی صعود دچار آلایش پوسته‌ای متوسط تا شدید شده‌اند. این توده‌ها با سرشت آهکی قلیایی از نوع I هستند که در موقعیت زمین‌ساختی فرورانش در ارتباط با کرانه قاره‌ای فعال تشکیل شده‌اند
کلیدواژه‌ها
شیمی کانی؛ گرانیتوئید؛ آهکی قلیایی؛ فرورانش؛ اردکان
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