دوره 26، شماره 4 - ( 10-1397 )                   جلد 26 شماره 4 صفحات 827-844 | برگشت به فهرست نسخه ها


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Baluchi S, Sadeghian M, Ghasemi H, Minggou Z, Li C, Yanbin Z. Mineral chemistry, geochemistry and isotope geochronology of kalateh region (NW of Khur): implication for Late Triassic magmatism of central Iran zone. www.ijcm.ir. 2019; 26 (4) :827-844
URL: http://ijcm.ir/article-1-1194-fa.html
بلوچی سولماز، صادقیان محمود، قاسمی حبیب ا...، مینگو جای، لی چیولی، یانبین ژانگ. شیمی کانی، زمین‌شیمی و سن‌ پرتوسنجی سنگ‌های آذرین نفوذی منطقه کلاته (شمال-غربی خور): شاهدی بر فعالیت ماگمایی تریاس پسین در پهنه ساختاری ایران مرکزی. مجله بلورشناسی و کانی شناسی ایران. 1397; 26 (4) :827-844

URL: http://ijcm.ir/article-1-1194-fa.html


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چکیده:   (71 مشاهده)
توده­های نفوذی دیوریتی و دایک­های آلکالی فلدسپار گرانیتی صورتی­رنگ منطقه کلاته (شمال­ غربی شهر خور)، سنگ­های مجموعه پی­سنگی نئوپروتروزوئیک­پایانی جندق- عروسان را قطع کرده­اند. بازدیدهای صحرایی، سنگ­نگاری و بررسی­های زمین­شیمیایی بیانگر ماهیت گرانیتوئیدی نوع  Iاین توده­های نفوذی، رابطه همزادی آن­ها با یکدیگر و ماهیت آهکی-قلیایی پتاسیم­متوسط تا پتاسیم ­بالای آن­هاست. ماگمای سازنده آن­ها، از ذوب­بخشی گوه گوشته­ای دگرنهاده دگرنهاد روی پهنه فرورانش ورقه فرورانده نئوتتیس، سرچشمه گرفته­ است. زایش ماگماهای مورد نظر، در یک محیط کششی پشت کمانی درون ورقه قاره­ای قرار گرفته بر روی پهنه فرورانش نئوتتیس صورت گرفته است. سن­سنجی U-Pb بر زیرکن­های جداشده از این سنگ­های دیوریتی و آلکالی فلدسپار گرانیتی نشانگر گستره سنی 6/1±9/213 تا 6/1±221 میلیون سال پیش (تریاس­ پسین) برای آن­هاست. این سنگ­های آذرین تظاهرات ماگمایی فاز کوهزادی سیمرین پیشین هستند.      
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نوع مطالعه: پژوهشي | موضوع مقاله: تخصصي
دریافت: ۱۳۹۷/۱۰/۸ | پذیرش: ۱۳۹۷/۱۰/۸ | انتشار: ۱۳۹۷/۱۰/۸

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