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ریزرخساره ها و محیط رسوبی سازند کژدمی در یال جنوبی تاقدیس خامی، شرق زون ایذه | ||
دوفصلنامه رسوب شناسی کاربردی | ||
دوره 11، شماره 22، دی 1402، صفحه 167-179 اصل مقاله (1.76 M) | ||
شناسه دیجیتال (DOI): 10.22084/psj.2023.27306.1383 | ||
نویسندگان | ||
کبری فتحی نژاد1؛ کبری میربیک سبزواری* 2؛ احمد عبیات2؛ سیامک بهاروند3؛ سید وحید شاهرخی3 | ||
1دانشجوی دکترا، گروه زمینشناسی، واحد خرمآباد، دانشگاه آزاد اسلامی، خرمآباد، ایران | ||
2استادیار گروه زمینشناسی، واحد خرمآباد، دانشگاه آزاد اسلامی، خرمآباد، ایران | ||
3دانشیار گروه زمینشناسی، واحد خرمآباد، دانشگاه آزاد اسلامی، خرمآباد، ایران | ||
چکیده | ||
در این مطالعه، ریزرخسارهها و محیط رسوبی سازند کژدمی در برش مارین (یال جنوبی تاقدیس خامی) در شرق زون ایذه، مورد بررسی قرار گرفته است. مطالعات رسوبشناسی منجر به شناسایی 6 ریزرخساره رسوبی در این سازند گردید. این ریزرخسارهها بهواسطه دارا بودن دانههای اسکلتی مانند رادیولرها، فرامینیفرهای پلانکتون، الیگوستژینیدها، سوزن اسفنج، آمونیت و خار اکینودرم، در یک محیط عمیق تشکیل شدهاند. فراوانی فسفات و وجود گلوکونیت، از دیگر ویژگیهای این ریزرخسارههاست. وجود لایههای شیلی آمونیتدار و غنی از مواد آلی، در تناوب به سنگآهکهای سازند کژدمی در برش مارین، مؤید عمیق بودن حوضه رسوبی سازند کژدمی میباشد. شواهد یاد شده، نشان از تهنشست ریزرخسارههای سازند کژدمی، در یک حوضه اینتراشلفی در این برش دارد. ریزرخسارههای شناسایی شده در برش مارین، در زیرمحیطهای حوضه و پلاتفرم بیرونی تشکیل شده و اثری از زیرمحیطهای کمعمقتر در آنها دیده نمیشود. | ||
کلیدواژهها | ||
مارین؛ حوضه رسوبی؛ اینتراشلف؛ کژدمی؛ ایذه | ||
مراجع | ||
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