خاستگاه سنگ های آتشفشانی مجموعه افیولیتی باغ چنار، شمال استان هرمزگان

نوع مقاله : مقاله پژوهشی

نویسندگان

گروه زمین شناسی، دانشکده علوم، دانشگاه هرمزگان، بندرعباس، ایران

چکیده

سنگ­های آتشفشانی منطقه باغ چنار در شمال شرق استان هرمزگان، شهرستان حاجی آباد واقع هستند. این سنگ­ها از نظر ساختاری در گستره­ی برخوردی با پهنه سنندج-سیرجان قرار دارند. مجموعه سنگ­های این منطقه دربردارنده گدازه­های بالشی، دایک­های ریزگابرویی، فرامافیک­ها و رسوب­های عمیق دریایی شامل آهک­های گودابه­ای و چرت­های رادیولاریتی و برخی میان لایه­های نازک رسوبی و سنگ­های دگرگونی است که در دوره فعالیت ماگمایی روی هم به صورت آمیزه رنگین انباشته شده­اند. بر اساس بررسی­های صحرایی، سنگ­های آتشفشانی این منطقه شامل بازالت و آندزیت بازالت هستند. بافت این سنگ­ها، پورفیری، شیشه­­ای پورفیری و گلومروپورفیری است. کانی­های اصلی تشکیل­دهنده این سنگ­ها پلاژیوکلاز و پیروکسن هستند. کانی­های فرعی و ثانویه نیز شامل کلسیت، کلریت و کانی­های کدر هستند که در یک زمینه شیشه­ای و ریز بلور قرار دارند. الگوی عناصر خاکی نادر و نمودارهای عنکبوتی بیانگر غنی­شدگی عناصر سنگ دوست درشت یون (LILE) و عناصر خاکی نادر سبک (LREE) و برخی از عناصر با شدت میدان بالا (HFSE) بوده که نشانگر شکل­گیری گدازه­های بالشی در گستره بازالت­های مناطق کششی هستند. بر اساس نمودارهای تعیین سری ماگمایی و محیط زمین­ساختی، سنگ­های مورد بررسی در گستره سری ماگمایی تولئیتی با خاستگاه پشته میان اقیانوسی قرار دارند. نتایج این پژوهش نشان می­دهد که سنگ­های آتشفشانی مجموعه افیولیتی باغ چنار از ماگمای تولئیت تشکیل شده­اند. این ماگما در یک محیط زمین­ساختی گسترش دریایی تشکیل شده است و فرآیندهای تکاملی ماگما در این مجموعه شامل تبلور جدایشی و آلودگی پوسته­ای بوده­اند.

کلیدواژه‌ها

عنوان مقاله [English]

Petrogenesis of volcanic rocks in Baghchenar ophiolitic complex, North of Hormozgan province

نویسندگان [English]

  • payam tavakoli
  • Mohammad Poosti
  • Gholamreza Gadami
Department of Geology, Faculty of Sciences, Hormozgan University, Bandarabas, Iran
چکیده [English]

The volcanic rocks of the Bagh Chenar region are located in the northeast of Hormozgan province, Hajiabad city. Structurally, these rocks are located in the collision range of Central Iran with the Sanandaj-Sirjan zone. The rock units in this area include pillow lava, microgabbro dyke, ultramafic, and deep marine sediments; including pelagic limestones and radiolarite cherts and some thin sedimentary layers and metamorphic rocks which have been piled on top of each other in the form of a colored mélange complex during the period of magmatic activity. Field studies show that this area's volcanic rocks include basalt and basalt andesite. The textures of these rocks are porphyry, hyaloporphyry, and glomeroporphyry. The main minerals include plagioclase and pyroxene as majors and minor and secondary minerals include calcite, chlorite, and opaque minerals located in a glassy and microcrystalline field. The pattern of rare earth elements (REE) and spider diagrams indicate the enrichment of LILE and LREE and some HFSE elements. According to the diagrams, the studied rocks are within the tholeiitic magmatic series with the origin of the mid-oceanic ridge. Also, based on the tectonic environment chart, the samples are located in the subduction zone or mid-ocean ridge. The results of this study show that the volcanic rocks of the Bagh Chenar ophiolite complex are composed of tholeiite magma. This magma was formed in a marine extension tectonic environment and the evolutionary processes of magma in this complex included fractional crystallization, magmatic isolation, and crustal contamination.
 

کلیدواژه‌ها [English]

  • volcanic
  • basalts
  • andesitbasalt
  • mid-ocean ridge
  • Bagh Chenar

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  • تاریخ دریافت: 16 دی 1402
  • تاریخ بازنگری: 09 بهمن 1402
  • تاریخ پذیرش: 14 فروردین 1403

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