سنگ‌زایی کوارتز دیوریت بروجرد بر پایه زمین‌شیمی عناصر اصلی و کمیاب کانی‌های پیروکسن و آمفیبول

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه پیام نور

2 دانشگاه میلان

3 دانشگاه دامغان

چکیده

مجموعه آذرین بروجرد (گرانیت، گرانودیوریت و کوارتزدیوریت) در نیمه شمالی نوار سنندج-سیرجان واقع است. در این پژوهش، فراوانی عناصر اصلی و کمیاب در کلینوپیروکسن و آمفیبول موجود در کوارتزدیوریت‌ اندازه‌گیری و ترکیب شیمیایی مذاب اولیه‌ای که این کانی‌ها از آن متبلور شده‌اند، محاسبه گردید. ترکیب شیمیایی این مذاب با کوارتز دیوریت بروجرد و همچنین کوارتز دیوریت و سنگ فرامافیک الیگودرز در کنار مجموعه بروجرد مقایسه شد. نتیجه این مقایسه به همراه مدلسازی‌های شیمیایی نشان می‌دهند که ماگمایی مشابه با کوارتز دیوریت الیگودرز دستخوش تبلور بخشی و هضم همزمان سنگ فرامافیک شده است. پیروکسن و آمفیبول از این ماگمای دگرگونه متبلور شده‌اند. سپس این ماگما با ماگمایی مشابه با کوارتز دیوریت الیگودرز آمیخته شده و کوارتز دیوریت بروجرد به وجود آمده است. نقش سنگ‌های فرامافیک در تشکیل کوارتز دیوریت بروجرد نشان می‌دهد که آنها با وجود رخنمون کم در سطح زمین، حجم قابل توجهی در اعماق دارند.

کلیدواژه‌ها

عنوان مقاله [English]

On the use of major and trace elements composition of pyroxene and amphibole in the genesis of Boroujerd quartz-diorite

نویسندگان [English]

  • Esna-Ashari 1
  • Tiepolo 2
  • Ghorbani 3
1
2
3
چکیده [English]

Boroujerd plutonic complex (granodiorite, quartz-diorite, and granite) is located in northern Sanandaj-Sirjan Zone. In this study, abundance of trace elements in clinopyroxene and amphibole from the quartz-diorite is measured and then composition of the parental melt of the minerals calculated. The melts are chemically compared with: 1- whole rock composition of the host quartz-diorite, and 2- quartz-diorite and ultramafic rock from the neighboring Aligoodarz plutonic complex. Geochemical modelings indicate that a melt chemically comparable with Aligoodarz quartz-diorite, affected by concurrent ultramafic rock assimilation and fractional crystallization to generate a new evolved melt from which pyroxene and amphibole crystallized. Then this melt mixed with Aligoodarz quartz-dioritic melt to generate a new melt that is comparable with Boroujerd quartz-diorite. The role that ultramafic rocks played in genesis of the Boroujerd quartz-diorite indicates that despite scarcity of ultramafic rocks on the surface, they are much more voluminous at depth.
 

کلیدواژه‌ها [English]

  • quartz-diorite
  • ultramafic rock
  • magma mixing
  • assimilation and fractional crystallization
  • Boroujerd
  • Sanandaj-Sirjan Zone

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  • تاریخ دریافت: 08 بهمن 1398
  • تاریخ بازنگری: 13 فروردین 1399
  • تاریخ پذیرش: 10 اردیبهشت 1399

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