سامانه مدیریت نشریات علمی دانشگاه دامغان

دامچین مشاک, سارا, ترکیان, اشرف, فورمن, تانیا. (1403). شیمی‌کانی و دما-فشار کانی‌های همزیست در سنگ‌های آندزیتی شمال سقز، شمال غرب ایران. مجله زمین شیمی ایران, 32(2), 339-358. doi: 10.61186/ijcm.32.2.339
سارا دامچین مشاک; اشرف ترکیان; تانیا فورمن. "شیمی‌کانی و دما-فشار کانی‌های همزیست در سنگ‌های آندزیتی شمال سقز، شمال غرب ایران". مجله زمین شیمی ایران, 32, 2, 1403, 339-358. doi: 10.61186/ijcm.32.2.339
دامچین مشاک, سارا, ترکیان, اشرف, فورمن, تانیا. (1403). 'شیمی‌کانی و دما-فشار کانی‌های همزیست در سنگ‌های آندزیتی شمال سقز، شمال غرب ایران', مجله زمین شیمی ایران, 32(2), pp. 339-358. doi: 10.61186/ijcm.32.2.339
دامچین مشاک, سارا, ترکیان, اشرف, فورمن, تانیا. شیمی‌کانی و دما-فشار کانی‌های همزیست در سنگ‌های آندزیتی شمال سقز، شمال غرب ایران. مجله زمین شیمی ایران, 1403; 32(2): 339-358. doi: 10.61186/ijcm.32.2.339

شیمی‌کانی و دما-فشار کانی‌های همزیست در سنگ‌های آندزیتی شمال سقز، شمال غرب ایران

مجله بلورشناسی و کانی شناسی ایران
مقاله 11، دوره 32، شماره 2 - شماره پیاپی 94، مرداد 1403، صفحه 339-358    اصل مقاله (2.14 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.61186/ijcm.32.2.339
نویسندگان
سارا دامچین مشاک1؛ اشرف ترکیان* 1؛ تانیا فورمن2
1گروه زمین شناسی، دانشکده علوم پایه، دانشگاه بوعلی سینا، همدان، ایران
2گروه علوم زمین، دانشگاه ایالتی پنسیلوانیا، دانشگاه پارک، پ.ا. 16802، امریکا
چکیده
منطقه سقز در شمال غرب ایران، در شمال پهنه سنندج - سیرجان و استان کردستان قرار دارد. سنگ‌های آندزیتی و آندزیت بازالتی آن از کانی‌های آمفیبول، پلاژیوکلاز، کلینوپیروکسن و ارتوپیروکسن تشکیل شده‌اند. ترکیب آمفیبول‌ها از منیزیو-‌هستینگزیت، منیزیو‌-هورنبلند تا چرماکیت–پارگازیت متفاوت است. ترکیب پیروکسن‌ها اوژیت- 39.33 En40.37-40.26 Fs20.49-13.89  Wo45.39 و انستاتیت  En59.863-71.04Fs26.083-36.850Wo 2.842-3.287است. مقدار آنورتیت پلاژیوکلازها از 23/39 تا 70/68 درصد نوسان دارد و ترکیب آنها بین آندزین تا لابرادوریت متغیر است. براساس دما و فشارسنجی بر پایه آلومینیوم در شبکه آمفیبول‎ها، دما و فشار تبلور °C 895-961 و  kbar11/2 – 59/4  بوده است. بر اساس مقدار Ti، دمای °C 800 تا 950 بدست آمده است. بررسی شیمی کانی کلینوپیروکسن نشان می‌دهد که انواع سنگ‌های آتشفشانی مورد بررسی در دمای 1100 تا 1250 درجه سانتی‌گراد و فشار 2 تا 10 کیلوبار متبلور شده‌اند. همچنین مقدار AlIV و Si بیانگر تبلور آمفیبول‌ها در فشارهای پایین است   که با مقدار AlIV/AlVI در پیروکسن‌های کم فشار تا فشار متوسط این پژوهش همخوانی دارد. افزون بر این، بررسی مقدار کاتیون‌های AlVI+2Ti+Cr و Na+AlIV در شبکه پیروکسن‌ها و مقادیر LogƒO2 و Fe# در شبکه آمفیبول‌ها چنین برداشت می‌گردد که آن‌ها در شرایط فشاربخشی بالا متبلور شده­اند.
کلیدواژه‌ها
پلاژیوکلاز؛ آمفیبول؛ پیروکسن؛ دما- فشارسنجی؛ فشاربخشی اکسیژن
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