ویژگی‌های زمین‌شیمیایی فعالیت ماگمایی قلیایی پتاسیمی شمال شرق قزوین (منطقه پرگه)

نوع مقاله : مقاله پژوهشی

نویسندگان

1 گروه زمین شناسی، دانشکده علوم پایه، دانشگاه لرستان، خرم آباد، ایران

2 گروه علوم زمین شناسی و زمین شناسی مهندسی، دانشگاه کوئینز، کینگستون، کانادا

3 گروه پترولوژی و کانی شناسی، دانشکده علوم، دانشگاه ریودژانیرو،ریودژانیرو، برزیل

چکیده

توده نفوذی پرگه در شمال شرق قزوین واقع شده است. سنگ­های نفوذی این توده بیشتر شامل مونزوگابرو و الیوین گابرو بوده که از نظر کانی­شناسی در بردارنده الیوین، کلینوپیروکسن، پلاژیوکلاز، بیوتیت و فلدسپار قلیایی هستند. از نظر زمین شیمیایی، این سنگ­ها دارای ویژگی‌ ماگماهای قلیایی پتاسیمی با غنی‌شدگی در عناصر سنگ دوست بزرگ یون ( Ba،U ،Pb ، Sr LILE:) و تهی شدگی در عناصر با شدت میدان بالا (HFSE: Nb, Ti, Zr) بوده که از این نظر شبیه فعالیت ماگمایی منطقه فرورانش و ماگماهای برآمده از گوشته هستند. الگوهای خاکی نادر (REE) بهنجار شده با کندریت غنی شدگی در عناصر خاکی نادر سبکLREE) )، با (La/Yb)N در گستره 58/8-43/4، و ناهنجاری‌های منفی جزئی (Eu/Eu* = 0.82-0.99) Eu را نشان می‌دهند. سنگ‌های گابرویی مورد بررسی برآمده از جدایش ماگمای اولیه ای هستند که از ذوب بخشی گوشته سنگ کره ای تهی شده با ترکیب اسپینل-پریدوتیت تشکیل شده‌اند. نسبت­های اولیه 87Sr/86Sr و 143Nd/144Nd  به ترتیب، (70493/0- 70525/0 و 51272/0-51269/0) با تشکیل ماگمای مادر در گوه گوشته­ای همخوانی دارند. مقادیرɛNd(i)  (47/1تا 92/1) در گستره مذاب­های برآمده از گوشته قرار دارند. بر پایه نتایج این پژوهش، پیشنهاد می‌شود که سنگ‌های نفوذی پرگه بخشی از کمربند ماگمایی البرز هستند که براساس داده­های زمین شیمیایی، محیط تشکیل آن­ها با یک محیط کششی پس از برخورد و پشت کمان همخوانی دارد.     

کلیدواژه‌ها

عنوان مقاله [English]

Geochemical characteristics of potassic alkaline magmatism of the northeastern Qazvin (Pargeh area)

نویسندگان [English]

  • nahid naseri 1
  • Reza Zarei Sahamieh 1
  • Matthew Leybourne 2
  • Anderson Costa dos Santos 3
  • Ahmad Ahmadi Khalaji 1
1 Department of Geology, Faculty of Sciences, Lorestan University, Khorramabad, Iran
2 Queen’s Facility for Isotope Research, Department of Geological Sciences and Geological Engineering, Queen’s University, Kingston, Ontario, Canada K7L 3N6
3 Rio de Janeiro State University (UERJ), Geology Faculty, Departamento de Mineralogia e Petrologia Ígnea (DMPI), Brazil
چکیده [English]

The Pargeh pluton is located in the northeast of Qazvin. The rocks of this pluton mainly include monzogabbro and olivine gabbro, which mineralogically contain olivine, clinopyroxene, plagioclase, biotite and alkali feldspar. Geochemically, they have features of potassic alkaline magmas with enrichment in large ion lithophile elements (LILE: Ba, U, Pb, Sr) and depletion in high field strength elements (HFSE: Nb, Ti, Zr), which are similar to subduction zone magmatism and mantle-derived magmas. Chondrite-normalized REE plots show enrichment in light REE (LREE) (4.43< (La/Yb) N <8.58)) and slight negative anomalies (Eu/Eu* = 0.82-0.99). The studied gabbroic rocks have resulted from fractional crystallization of a parental magma which formed by partial melting of depleted lithospheric mantle with spinel-peridotite composition. The primary ratios of 87Sr/86Sr and 143Nd/144Nd (0.70493-0.70525 and 0.51272-0.51269) are compatible with the parental magma formation in the mantle wedge. The values of ɛNd(i) (1.47 to 1.92) are in the range of mantle-derived melts. We suggest that Pargeh gabbroic rocks are part of the Alborz magmatic belt, which according to the geochemical data, their tectonic setting is consistent with a post-collisional, back-arc extensional environment.

کلیدواژه‌ها [English]

  • Potassic alkaline magmatism
  • Sr-Nd isotope
  • Post-collision
  • Pargeh
  • Iran

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  • تاریخ دریافت: 03 تیر 1402
  • تاریخ بازنگری: 06 مرداد 1402
  • تاریخ پذیرش: 30 مرداد 1402

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