سنگ‌نگاری، زمین‌شیمی و خاستگاه بازالت‌های پلیوکواترنر غازان، شمال غرب ارومیه

نوع مقاله : مقاله پژوهشی

نویسندگان

دانشگاه ارومیه

چکیده

سنگ­های آتشفشانی پلیوکواترنر در شمالی­ترین بخش پهنه سنندج – سیرجان، در شمال­ غرب ارومیه رخنمون گسترده­ای دارند. بلورهای اولیوین+ پیروکسن± پلاژیوکلاز فاز اصلی کانیایی هستند که هم بصورت درشت بلور و هم ریز بلور با کانی­های فرعی دیگر در متن سنگ وجود دارند. این سنگ­ها بافت­های پورفیری، ریزسنگی پورفیری، شیشه ای پورفیری، انبوهه پورفیری و حفره­ای دارند. از نظر زمین­شیمی، سنگ خاستگاه این سنگ­ها با طیف ترکیبی تراکی­بازالت تا تراکی­آندزیت بازالت وابسته به سری­های قلیایی هستند. نمودارهای عنکبوتی عناصر کمیاب بهنجار شده به گوشته و کندریت غنی شدگی در عناصر خاکی نادر سبک (LREE) و عناصر سنگ دوست بزرگ یون (LILE) نسبت به عناصر نادر خاکی سنگین (HREE) و عناصر با شدت میدان بالا HFSE نشان می­دهند. در این نمودارها، بی­هنجاری منفی در Nb، Ta، P < /span>، Rb، Zr و Ti و بی­هنجاری مثبت در Pb، La، U،  Nd،Th ، Yb و Cs وجود دارد. این ویژگی­ها بهمراه نمودارهای زمین­ساختی نشان می­دهند که فعالیت ماگمایی پلیو-کواترنر غازان در پهنه­های کمان­های ماگمایی پس از برخوردی رخ داده­اند.    

کلیدواژه‌ها

عنوان مقاله [English]

Petrography, geochemistry and source of Ghazan Plio-Quaternary basalts, NW Urmia

نویسندگان [English]

  • Asadpou
  • Ahangari
چکیده [English]

The volcanic rocks with the Plio-Quaternary age, are exposed in the northern part of the Sanandaj-Sirjan zone, in northwest Urmia. The main mineral phases are olivin + clinopyroxene ± plagioclase, that are present as both phenocrysts to microcrystalline with other minor minerals. The dominant textures of these rocks are porphyry, microlithic porphyry, hyalo-porphyry, glomeroporphyritic and vesicular. Based on geochemistry, the parent magma of these rocks are in the range of trachy-basalt to basaltic trachy andesite, belonging to the alkaline magmatic series. The mantel and chondrite normalised patterns of rare earth elements indicates the enrichment of LILE and LREE as well as the depletion of HFSE and HREE.The spider diagrams show a negative anomaly in Nb, Ta, P, Rb, Zr and Ti and positive anomaly in Pb, La, U, Nd, Th and Cs. These geochemical parameters and tectonic diagrams show that the Plio-Quaternary alkaline magmatism were formed in the post-collision arcs.
 

کلیدواژه‌ها [English]

  • Geochemistry
  • Plio-Quaternary basalt
  • post-collision arc
  • Ghazan
  • Urmia

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  • تاریخ دریافت: 25 اردیبهشت 1400
  • تاریخ بازنگری: 29 خرداد 1400
  • تاریخ پذیرش: 07 تیر 1400

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