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

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه صنعتی شاهرود

2 انجمن علوم چین

چکیده

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.      

کلیدواژه‌ها

عنوان مقاله [English]

Mineral chemistry, geochemistry and isotope geochronology of kalateh region (NW of Khur): implication for Late Triassic magmatism of central Iran zone

نویسندگان [English]

  • Solmaz Baluchi 1
  • Mahmmod Sadeghian 1
  • Habib Ghasemi 1
  • Zh Minggou 2
  • Chioli Li 2
  • Zh Yanbin 2
1 Shahrood University of Technology
2 Chinese Academy of Science
چکیده [English]

Dioritic plutons and pinkish alkali-feldspar granitic dikes of Kalateh area (northwest of Khur city) intruded in Neoproterozoic basemental of Jandagh- Arousan complex. Field observations, petrography and geochemical studies indicate that these intrusive rocks have I-type nature and belong to medium-high K calc-alkaline granitiods and also have genetically relationship with each other. Their parental magmas produced by partial melting of metasomatized mantle wedge which was located above the subducted Neotethyan oceanic slab. The mentioned magmas generated in an intracontinental back arc extensional setting in relation to the subduction of oceanic Neotethys slab. U-Pb dating results on separated zircon from dioritic and alkali-feldspar granitic rocks indicated 213.9 ± 1.6 to 221.16 ± 1.6 Ma interval age (corresponding to Late Triassic). These igneous rocks are indications of magmatic manifestations of Early Cimmerian Orogeny.

کلیدواژه‌ها [English]

  • diorite
  • alkali-feldspar granite
  • Late Triassic
  • Neotethys subduction
  • Kalateh
  • Khur

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  • تاریخ دریافت: 06 دی 1396
  • تاریخ بازنگری: 07 بهمن 1396
  • تاریخ پذیرش: 12 اسفند 1396

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