سامانه مدیریت نشریات علمی دانشگاه دامغان

پیغمبری, سیما. (1397). ویژگی‌های زمین‌ساختی ماگمایی گابروئیدهای افیولیتی جنوب ارزوئیه (جنوب بافت، استان کرمان) بر پایه شیمی کانی کلینوپیروکسن. مجله زمین شیمی ایران, 26(2), 301-314. doi: 10.29252/ijcm.26.2.301
سیما پیغمبری. "ویژگی‌های زمین‌ساختی ماگمایی گابروئیدهای افیولیتی جنوب ارزوئیه (جنوب بافت، استان کرمان) بر پایه شیمی کانی کلینوپیروکسن". مجله زمین شیمی ایران, 26, 2, 1397, 301-314. doi: 10.29252/ijcm.26.2.301
پیغمبری, سیما. (1397). 'ویژگی‌های زمین‌ساختی ماگمایی گابروئیدهای افیولیتی جنوب ارزوئیه (جنوب بافت، استان کرمان) بر پایه شیمی کانی کلینوپیروکسن', مجله زمین شیمی ایران, 26(2), pp. 301-314. doi: 10.29252/ijcm.26.2.301
پیغمبری, سیما. ویژگی‌های زمین‌ساختی ماگمایی گابروئیدهای افیولیتی جنوب ارزوئیه (جنوب بافت، استان کرمان) بر پایه شیمی کانی کلینوپیروکسن. مجله زمین شیمی ایران, 1397; 26(2): 301-314. doi: 10.29252/ijcm.26.2.301

ویژگی‌های زمین‌ساختی ماگمایی گابروئیدهای افیولیتی جنوب ارزوئیه (جنوب بافت، استان کرمان) بر پایه شیمی کانی کلینوپیروکسن

مجله بلورشناسی و کانی شناسی ایران
مقاله 4، دوره 26، شماره 2 - شماره پیاپی 72، تیر 1397، صفحه 301-314    اصل مقاله (4.65 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.29252/ijcm.26.2.301
نویسنده
سیما پیغمبری*
دانشگاه پیام نور
چکیده
سری­های سنگی مافیک-فرامافیک لایه­ای جنوب ارزوئیه واقع در جنوب بافت (استان کرمان) شامل سنگ­های فرامافیک پلاژیوکلاز­دار (دربردارنده ترکیب مدال الیوین، کلینوپیروکسن، ارتوپیروکسن و پلاژیوکلاز)، الیوین گابرو (شامل پلاژیوکلاز، الیوین، ارتوپیروکسن، کلینوپیروکسن)، و انواع گابرونوریت­ها (دربردارنده ارتوپیروکسن، کلینوپیروکسن، آمفیبول و پلاژیوکلاز که در قسمت­های تیره و روشن مقدار پلاژیوکلاز متفاوت است) است که بخش مافیک همبافت آمیزه رنگین ارزوئیه را تشکیل می­دهند. تجزیه نقطه­ای انجام شده بر روی کلینوپیروکسن موجود در این سنگ­ها بیانگر وجود کلینوپیروکسن از نوع دیوپسید با Mg# به نسبت بالا (75/0-88/0) است. محاسبات دما و فشارسنجی کلینوپیروکسن­ها کمینه دمای تبلور معادل  ºC783 تا 975 و فشار 4/1 تا 6/3 کیلوبار را نشان می­دهد. از نظر زمین­ساختی ماگمایی ترکیب گدازه تشکیل دهنده این کلینوپیروکسن­ها، تولئیتی تا بونینیتی است که در یک محیط قوس شکل گرفته­اند. بدین ترتیب می­توان سری­های سنگی فرامافیک و مافیک لایه­ای ارزوئیه را بخشی از مجموعه­های افیولیتی در نظر گرفت که در منطقه فرورانش واقع شده­اند.     
کلیدواژه‌ها
زمین‌ساختی ماگمایی؛ شیمی کانی؛ کلینوپیروکسن؛ فرامافیک و مافیک لایه‌ای؛ افیولیت؛ ارزوئیه
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