فصلنامه علمی علوم زمین

فصلنامه علمی علوم زمین

مقایسه رسوب‌شناسی و تغییرات محیط رسوبی سازند شوریجه در بخش‌های مرکزی و خاور حوضه کپه‌داغ، شمال خاور ایران

نوع مقاله : مقاله پژوهشی

نویسندگان
زهرا اسماعیلی خوشمردان
محمد حسین محمودی قرائی
اسداله محبوبی
سید رضا موسوی حرمی
گروه زمین‌شناسی، دانشکده علوم، دانشگاه فردوسی مشهد، مشهد، ایران
10.22071/gsj.2025.520806.2194
چکیده
سازند شوریجه در برش‌های رادکان و بید‌سوخته در شمال خاور ایران به طور عمده از نهشته‌های کربناته و سیلیسی آواری تشکیل شده است؛ به گونه‌ای که به سمت باختر از رخساره‌های سیلیسی آواری کاسته شده و بر رخساره‌های کربناته افزوده می‌شود. مطالعه رخساره‌های آواری به معرفی 7 رخساره دانه‌درشت (Gmm, Gms, Gci, Gcm, Gmg, Gt, Gh)، 6 رخساره دانه‌متوسط (Sr, Sm, Sh, Sp, St, Sl)، 2 رخساره دانه‌ریز (Fm, Fl) و سیلتستون انجامید. همچنین مطالعه رخساره‌های کربناته به وجود 2 رخساره میان‌کشندی (بین جزرو‌مدی) (دولومیت ماسه‌ای بایوکلستی، دولستون) و 17 رخساره‌ متنوع زیرکشندی دلالت دارد. با توجه به ویژگی‌های رخساره‌ای و شکل هندسی لایه‌ها، در محیط‌های رسوبی متنوعی از جمله: قاره‌ای  (Flood plain Point bar, Chanal,)، کشندی، لاگون، سد و دریای‌باز تفکیک می‌شوند. سه سکانس رسوبی در نهشته‌های رسوبی سازند شوریجه براساس رخساره‌ها و سطوح اصلی چینه‌نگاری شناسایی شده است. تنوع رخساره‌ها در این سازند حاصل فاز خشکی‌زایی، تغییرات توپوگرافی و تغییرات جهانی سطح آب دریا در اواخر ژوراسیک پسین و کرتاسه پیشین است.
کلیدواژه‌ها
محیط‌رسوبی
چینه‌نگاری‌ سکانسی
سازند‌ شوریجه
کپه داغ
موضوعات
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فصلنامه علمی علوم زمین
دوره 35، شماره 3 - شماره پیاپی 137
پاییز1404، سال سی‌و پنجم، شماره 3، پیاپی 137
پاییز 1404
صفحه 41-62