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برزگری, لیلا, قاسمی, حبیب الله, رضائی کهخائی, مهدی. (1404). نرخ هسته‌بندی و رشد بلورهای پلاژیوکلاز و پیروکسن در سنگ‌های آندزیتی و بازالتی منطقه عباس آباد، شرق شاهرود. مجله زمین شیمی ایران, 26(1), 63-78. doi: 10.29252/ijcm.26.1.63
لیلا برزگری; حبیب الله قاسمی; مهدی رضائی کهخائی. "نرخ هسته‌بندی و رشد بلورهای پلاژیوکلاز و پیروکسن در سنگ‌های آندزیتی و بازالتی منطقه عباس آباد، شرق شاهرود". مجله زمین شیمی ایران, 26, 1, 1404, 63-78. doi: 10.29252/ijcm.26.1.63
برزگری, لیلا, قاسمی, حبیب الله, رضائی کهخائی, مهدی. (1404). 'نرخ هسته‌بندی و رشد بلورهای پلاژیوکلاز و پیروکسن در سنگ‌های آندزیتی و بازالتی منطقه عباس آباد، شرق شاهرود', مجله زمین شیمی ایران, 26(1), pp. 63-78. doi: 10.29252/ijcm.26.1.63
برزگری, لیلا, قاسمی, حبیب الله, رضائی کهخائی, مهدی. نرخ هسته‌بندی و رشد بلورهای پلاژیوکلاز و پیروکسن در سنگ‌های آندزیتی و بازالتی منطقه عباس آباد، شرق شاهرود. مجله زمین شیمی ایران, 1404; 26(1): 63-78. doi: 10.29252/ijcm.26.1.63

نرخ هسته‌بندی و رشد بلورهای پلاژیوکلاز و پیروکسن در سنگ‌های آندزیتی و بازالتی منطقه عباس آباد، شرق شاهرود

مجله بلورشناسی و کانی شناسی ایران
مقاله 5، دوره 26، شماره 1 - شماره پیاپی 69، فروردین 1397، صفحه 63-78    اصل مقاله (4.38 M)
شناسه دیجیتال (DOI): 10.29252/ijcm.26.1.63
نویسندگان
لیلا برزگری؛ حبیب الله قاسمی؛ مهدی رضائی کهخائی*
دانشگاه صنعتی شاهرود
چکیده
نوار ماگمایی ائوسن کاهک- عباس­آباد، در کرانه شمال شرقی پهنه ساختاری ایران مرکزی، از داورزن در غرب سبزوار تا میامی در شرق شاهرود امتداد دارد. واحدهای سنگی این نوار شامل تناوبی از سنگ­های آتشفشانی بازی - حدواسط (الیوین بازالت، بازالت، تراکی­بازالت، تراکی­آندزی بازالت، تراکی­آندزیت و آندزیت) و سنگ­های آذرآواری –رسوبی (انواع توف، بِرِش، آگلومرا، ماسه­سنگ، ­شیل، کنگلومرا، سنگ آهک نومولیتی و سنگ آهک توفی) به سن ائوسن میانی – پسین و سنگ­های رسوبی الگیوسن و کواترنری هستند. سنگ­های آتشفشانی این نوار، یک سری تفریقی پیوسته با خاستگاه مشترک از یک ماگمای والد بازالتی هستند. گدازه­های بازالتی– آندزیتی منطقه از آنجا که از نوع پیروکسن پورفیری، پلاژیوکلاز پورفیری و پیروکسن- پلاژیوکلاز پورفیری هستند، نمونه­های مناسبی برای بررسی­های توزیع اندازه بلور (CSD) به­شمار می­روند. براساس نتایج این پژوهش، درشت بلور­های پلاژیوکلاز و پیروکسن موجود در سنگ­های آتشفشانی منطقه، به ترتیب در گستره زمانی86 تا 118 سال و با نرخ هسته­بندی از 10-10× 48/1- تا 10-10× 56/1 میلی­متر بر ثانیه و در گستره­ زمانی 104×21/3 تا 104 × 3/6 ثانیه و با نرخ هسته­بندی از  5-10× 55/0 تا  5-10× 2 میلی متر بر ثانیه در آشیانه ماگمایی رشد کرده­اند.     
کلیدواژه‌ها
توزیع اندازه بلور (CSD)؛ سنگ‎های بازالتی- آندزیتی؛ عباس‌آباد؛ شاهرود
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