معرفی ایکنوفاسیس های قاره ای از نهشته های آبرفتی رودخانه ای نئوژن شهر بیرجند

نویسنده

استادیار گروه زمین‌شناسی، دانشکده علوم، دانشگاه بیرجند، بیرجند، ایران

چکیده

در سال­های اخیر ایکنولوژی قاره­ای اهمیت زیادی در مطالعات چینه­شناسی، آنالیز حوضه و جغرافیای دیرینه پیدا کرده و کاربرد زیادی در شناخت پارامترهای محیطی و شرایط زیستی گذشته دارد. منطقه مورد مطالعه در شهر بیرجند جزء زون رسوبی- ساختاری خاور ایران محسوب می­شود و شامل نهشته­های رسوبی آبرفتی به سن نئوژن است. بر اساس مطالعات قبلی، نهشته­های آبرفتی فوق شامل رخساره­های کنگلومرایی، ماسه­سنگی و گل­سنگی هستند که بر مبنای اختصاصات بافتی و ساختمان­های رسوبی خود در سیستم رودخانه­ای بر­جای گذاشته شده­اند. رخساره­های سنگی، مجموعه­های رخساره­ای و فراوانی نهشته­های جریان گراویته­ای رسوب و رسوبات پرکننده کانال در نهشته­های آبرفتی مورد مطالعه نشان­دهنده وجود یک سیستم رودخانه­ای بریده بریده نزدیک به منشأ در زمان نئوژن است. مشاهدات صحرایی نهشته­های ماسه­ای و گلی پادگانه­های آبرفتی مورد مطالعه نشان­دهنده وجود اثرفسیل­های قاره­ای در این رسوبات است. بر اساس اثرفسیل­های مشاهده شده در این رسوبات، دو ایکنوفاسیس Coprinisphaera و Skolithos و شش ایکنوجنس متمایز در این نهشته­های قاره­ای قابل تفکیک است که نهشته­شدن این رسوبات در بخش­های مجاور کانال فعال و دشت­سیلابی سیستم رودخانه­ای را تأیید می­کند.

کلیدواژه‌ها


عنوان مقاله [English]

Introduction of continental ichnofacies from Neogene alluvial deposits of Birjand city

نویسنده [English]

  • M. Mortazavi Mehrizi
Assist. Prof., Dept., of Geology, Faculty of Sciences, University of Birjand, Birjand, Iran
چکیده [English]

In recent years, continental ichnology has gained great importance in the stratigraphy, basin analysis and paleogeography studies and widely used in understanding environmental parameters and paleoecological conditions. The study area in the Birjand city is a part of the sedimentary-structural zone of eastern Iran and includes alluvial sedimentary deposits with Neogene age. Based on the previous studies, the above-mentioned alluvial deposits include conglomerate, sandstone and mudstone lithofacies which were deposited in the fluvial system based on their textural features and sedimentary structures. Lithofacies, facies associations and the abundance of sediment gravity flow and channel-fill deposits, in the studied alluvial deposits indicate the existence of a braided fluvial system close to the source during the Neogene time. Field observations of the sand and mud deposits of the studied alluvial terraces indicate the presence of continental trace fossils in these sediments. Based on the observed burrows of these sediments, two Coprinisphaera and Skolithos ichnofacies and six distinct ichnogenus can be distinguished in these continental deposits, which confirm the deposition of these sediments in the adjacent parts of active channel and floodplain of fluvial system.   

کلیدواژه‌ها [English]

  • Coprinisphaera ichnofacies
  • Skolithos ichnofacies
  • Alluvial terraces
  • Neogene
  • North of Birjand
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