بررسی روند تحولات تکتونیکی-رسوبی مرتبط با دیاپیر نمکی هندون (ناحیه بندرعباس) با استفاده از سکانس‌های هالوکینتیکی در رخنمون‌های سطحی

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشجوی دکترا، گروه زمین شناسی، دانشکده علوم پایه، دانشگاه هرمزگان، بندرعباس، ایران

2 دانشیار، گروه زمین شناسی ، دانشکده علوم پایه، دانشگاه هرمزگان، بندرعباس، ایران

3 دکترا، مدیریت اکتشاف شرکت ملی نفت ایران، تهران، ایران

4 استادیار، گروه زمین شناسی، دانشکده علوم پایه، دانشگاه هرمزگان، بندرعباس، ایران

چکیده

سامانه‌های رسوبی مرتبط با دیاپیرهای نمکی آزمایشگاه‌های طبیعی هستند که بررسی چینه‌های مرتبط با فعالیت نمک را براساس داده‌های زیرسطحی و به‌ویژه داده‌های سطحی فراهم می‌نمایند. در این سامانه‌ها، چینه‌های رشدی هالوکینتیکی، تغییرات ضخامتی و رخساره‌ای را به صورت برش‌های هالوکینتیکی، اشکال هندسی گوه‌ای و هوک و همچنین پهنه‌های دیاژنتیکی متنوع نشان می‌دهند. بدین جهت، دیاپیر نمکی هندون به عنوان یک دیاپیر غیرفعال در ناحیه بندرعباس برای این مطالعه انتخاب شد. رخنمون‌های سطحی عالی که پیرامون این دیاپیر نمکی وجود دارد امکان بررسی‌های جزئی‌تر تکتونیکی-رسوبی و تقابل نمک-رسوب را فراهم می‌نماید که می‌تواند همچون یک مدل آنالوگ در سایر پژوهش‌های سطحی و زیرسطحی اکتشافات هیدروکربوری حوضه زاگرس که شرایط رسوبگذاری مشابهی دارند، مورد استفاده قرار گیرد. چینه‌نگاری رسوبات پیرامون دیاپیر نمکی هندون شامل رسوبات برجای کرتاسه پسین تا عهدحاضر می‌باشد که تأثیر صعود دیاپیر نمکی بر این توالی‌ها از نظر زمانی و مکانی متفاوت است. عملکرد هالوکینسیز با هندسه‌های هوکی در سازند شیلی پابده پالئوسن-ائوسن زیرین نمایان می‌گردد. سپس بیشترین تأثیر حرکت و جریان نمک با تشکیل ورقه و باله‌های نمکی در کربنات‌های ائوسن میانی سازند جهرم رخ داده است که به ‌صورت تغییرات جانبی رخساره‌ای، هندسی (گوه‌ و هوک)، ضخامتی و دیاژنتیکی دیده می‌شود.

کلیدواژه‌ها

موضوعات


کتابنگاری
فیضی، ا.، نائیجی، م.ر.، پیریائی، ع.ر.، سرادقی صوفیانی، ح. و همت، س.، 1392- موقعیت تکتونیکی-رسوبی نهشته‌های آلبین در برش‌های سطحی کوه‌های گنو، انگورو و خمیر (ناحیه بندرعباس)، ماهنامه اکتشاف و تولید، شماره 99، ص. 75-68. 
مطیعی، ه.، 1374- زمین‌شناسی نفت زاگرس 1 و 2، سازمان زمین‌شناسی کشور، طرح تدوین کتاب زمین‌شناسی ایران، شماره 25: 1043 ص. 

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