ویژگی‌های زمین‌ساختی ماگمایی گابروئیدهای افیولیتی جنوب ارزوئیه (جنوب بافت، استان کرمان) بر پایه شیمی کانی کلینوپیروکسن

نوع مقاله : مقاله پژوهشی

نویسنده

دانشگاه پیام نور

چکیده

سری­های سنگی مافیک-فرامافیک لایه­ای جنوب ارزوئیه واقع در جنوب بافت (استان کرمان) شامل سنگ­های فرامافیک پلاژیوکلاز­دار (دربردارنده ترکیب مدال الیوین، کلینوپیروکسن، ارتوپیروکسن و پلاژیوکلاز)، الیوین گابرو (شامل پلاژیوکلاز، الیوین، ارتوپیروکسن، کلینوپیروکسن)، و انواع گابرونوریت­ها (دربردارنده ارتوپیروکسن، کلینوپیروکسن، آمفیبول و پلاژیوکلاز که در قسمت­های تیره و روشن مقدار پلاژیوکلاز متفاوت است) است که بخش مافیک همبافت آمیزه رنگین ارزوئیه را تشکیل می­دهند. تجزیه نقطه­ای انجام شده بر روی کلینوپیروکسن موجود در این سنگ­ها بیانگر وجود کلینوپیروکسن از نوع دیوپسید با Mg# به نسبت بالا (75/0-88/0) است. محاسبات دما و فشارسنجی کلینوپیروکسن­ها کمینه دمای تبلور معادل  ºC783 تا 975 و فشار 4/1 تا 6/3 کیلوبار را نشان می­دهد. از نظر زمین­ساختی ماگمایی ترکیب گدازه تشکیل دهنده این کلینوپیروکسن­ها، تولئیتی تا بونینیتی است که در یک محیط قوس شکل گرفته­اند. بدین ترتیب می­توان سری­های سنگی فرامافیک و مافیک لایه­ای ارزوئیه را بخشی از مجموعه­های افیولیتی در نظر گرفت که در منطقه فرورانش واقع شده­اند.     

کلیدواژه‌ها

عنوان مقاله [English]

Tectonomagmatic characteristics of ophiolitic gabbroids from south Orzuieh (south of Baft, Kerman) ophiolite complex: insights from clinopyroxene chemistry.

چکیده [English]

Mafic and ultramafic layered rocks located in south of Orzuieh (Baft, Kerman province), consist of plagioclase bearing ultramafic rocks (including olivine, orthopyroxene , clinopyroxene and plagioclase), olivine gabbros (including plagioclase, olivine, orthopyroxene and clinopyroxene) and gabbronorites (including plagioclase, orthopyroxene and clinopyroxene and amphibole) and constitute the mafic parts of the Orzuieh colored mélange complex. Mineral chemistry of clinopyroxene show diopside end-member which have Mg# ranging from 0.75 to 0.88. According to geothermobarometric calculations, temperatures change from 783 to 975ºC and pressure conditions vary from 1.4 to 3.6 kbar. Tectono-magmatic considerations show that these clinopyroxenes have been crystallized from tholeiitic to bonintic magmas which have already formed in an arc environment. Therefore, it could be considered that Orzuieh layered ultramafic and mafic rock series are some parts of ophiolitic complexes which occurred in a subduction setting.

کلیدواژه‌ها [English]

  • Tectonomagmatic
  • Mineral chemistry
  • clinopyroxene
  • layered ultramafic and mafic
  • ophiolite
  • Orzuieh

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  • تاریخ دریافت: 06 تیر 1396
  • تاریخ بازنگری: 08 مرداد 1396
  • تاریخ پذیرش: 12 شهریور 1396

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