سامانه مدیریت نشریات علمی دانشگاه دامغان

نظری, مسعود, آرین, محمد علی, سلگی, علی, زارعی سهامیه, رضا, یزدی, عبداله. (1403). بررسی شیمی کانی و دما فشار سنجی درشت بلور‌های پلاژیوکلاز، پیروکسن و آمفیبول سنگ‌های آتشفشانی حسین آباد (جنوب شرقی ابهر). مجله زمین شیمی ایران, 32(2), 197-214. doi: 10.61186/ijcm.32.2.197
مسعود نظری; محمد علی آرین; علی سلگی; رضا زارعی سهامیه; عبداله یزدی. "بررسی شیمی کانی و دما فشار سنجی درشت بلور‌های پلاژیوکلاز، پیروکسن و آمفیبول سنگ‌های آتشفشانی حسین آباد (جنوب شرقی ابهر)". مجله زمین شیمی ایران, 32, 2, 1403, 197-214. doi: 10.61186/ijcm.32.2.197
نظری, مسعود, آرین, محمد علی, سلگی, علی, زارعی سهامیه, رضا, یزدی, عبداله. (1403). 'بررسی شیمی کانی و دما فشار سنجی درشت بلور‌های پلاژیوکلاز، پیروکسن و آمفیبول سنگ‌های آتشفشانی حسین آباد (جنوب شرقی ابهر)', مجله زمین شیمی ایران, 32(2), pp. 197-214. doi: 10.61186/ijcm.32.2.197
نظری, مسعود, آرین, محمد علی, سلگی, علی, زارعی سهامیه, رضا, یزدی, عبداله. بررسی شیمی کانی و دما فشار سنجی درشت بلور‌های پلاژیوکلاز، پیروکسن و آمفیبول سنگ‌های آتشفشانی حسین آباد (جنوب شرقی ابهر). مجله زمین شیمی ایران, 1403; 32(2): 197-214. doi: 10.61186/ijcm.32.2.197

بررسی شیمی کانی و دما فشار سنجی درشت بلور‌های پلاژیوکلاز، پیروکسن و آمفیبول سنگ‌های آتشفشانی حسین آباد (جنوب شرقی ابهر)

مجله بلورشناسی و کانی شناسی ایران
مقاله 1، دوره 32، شماره 2 - شماره پیاپی 94، مرداد 1403، صفحه 197-214    اصل مقاله (1.73 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.61186/ijcm.32.2.197
نویسندگان
مسعود نظری1؛ محمد علی آرین* 2؛ علی سلگی1؛ رضا زارعی سهامیه3؛ عبداله یزدی4
1گروه زمین شناسی، واحد علوم و تحقیقات، دانشگاه آزاد اسلامی، تهران، ایران
2گروه زمین شناسی، واحد تهران شمال، دانشگاه آزاد اسلامی، تهران، ایران
3گروه زمین شناسی، دانشگاه لرستان، خرم آباد، ایران
4گروه زمین شناسی، واحد کهنوج، دانشگاه آزاد اسلامی، کهنوج، ایران
چکیده
منطقه حسین آباد در 120 کیلومتری  جنوب شرقی زنجان واقع است. سنگ­های آتشفشانی در این منطقه دارای سن ائوسن و جوانتر از آن هستند. سنگ­های آتشفشانی طیفی از گدازه­های داسیتی، تراکی آندزیتی و آندزیتی به همراه توف را شامل می­شوند. از نظر کانی­شناسی، سنگ­های آتشفشانی مورد بررسی دارای کوارتز، فلدسپات قلیایی، پلاژیوکلاز فراوان، پیروکسن و آمفیبول هستند. فلدسپات قلیایی از نوع سانیدین و پلاژیوکلازها از نوع الیگوکلاز و آندزین هستند. بافت­های پورفیری، پورفیری ریزسنگی، گلومرو پورفیری و خال خال بافت در این سنگ­ها غالب هستند. بررسی شیمی کانی­های سنگ­های منطقه نشان می­دهد که ترکیب کلینوپیروکسن­های این سنگ­ها از انواع دیوپسید و اوژیت است. آمفیبول موجود در این سنگ­ها از نوع ماگمایی و کلسیمی و دارای ترکیب شیمیایی پارگازیت است. بر اساس نمودارهای تعیین نوع ماگما، ماگمای سازنده سنگ­های آتشفشانی منطقه مورد بررسی قلیایی است. نمودارهای دما-فشارسنجی بر پایهی ترکیب پلاژیوکلاز، پیروکسن و آمفیبول نشان­دهنده دمای 700 تا 750 درجه سانتیگراد و فشار 5 تا 6.5 کیلوبار هستندکه با ژرفای پوسته میانی-زیرین همخوانی دارد. از این رو، این سنگ­ها در یک کرانه فعال قاره­ای تشکیل شده­اند.
کلیدواژه‌ها
دما فشارسنجی؛ آمفیبول؛ پلاژیوکلاز؛ سنگ‌های آتشفشانی؛ ابهر
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