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محیط رسوبی و تاریخچه دیاژنز سازند فهلیان در تاقدیس لار، جنوب زون ایذه | ||
دوفصلنامه رسوب شناسی کاربردی | ||
مقاله 1، دوره 3، شماره 6، آذر 1394، صفحه 1-25 اصل مقاله (2.91 M) | ||
نوع مقاله: مقاله پژوهشی | ||
نویسندگان | ||
حسین نوری* ؛ حسین رحیمپور بناب | ||
دانشکده زمینشناسی، دانشگاه تهران، تهران | ||
چکیده | ||
سازند فهلیان شامل توالی کربناته نسبتاً ضخیمی از گروه خامی به سن نئوکومین – بارمین میباشد. مطالعات صورت گرفته بر روی این سازند در تاقدیس لار واقع در زون ایذه، منجر به شناسایی 25 ریزرخساره در 4 کمربند رخسارهای شد. در سازند فهلیان بقایای موجودات چارچوبساز نظیر مرجانهای هرماتیپیک و جلبکها از گسترش بسیار اندکی برخوردار بوده و رخسارههای دانهپشتیبان شول دارای گسترش بسیار زیاد و مطلوبی هستند. محیط رسوبگذاری سازند فهلیان در تاقدیس لار رمپ کربناته هموکلینال تعیین گردید و با توجه به گسترش رخسارههای دانه غالب، احتمال میرود سازند فهلیان در یک رمپ رو به باد نهشته شده است. به نظر میرسد سازند فهلیان در منطقه مورد بررسی به صورت مجموعههای ساحل – سدی (Barrier – Bank complexes) تشکیل شده است و با توجه به گسترش رخسارههای گرینستون بایوکلستی، بایوکلست-پلوئید وکستون-پکستون، ماسهسنگهای آهکی و وجود استروماتوپوراید در سازند فهلیان، و ضخامت قابلملاحظهای رخساره شول احتمال میرود محیط رسوبی سازند فهلیان تحت تأثیر امواج قرار داشته است. از مهمترین فرایندهای دیاژنزی موثر در سازند فهلیان در تاقدیس لار میتوان به انحلال، میکرایتی شدن، تراکم، دولومیتی شدن، دولومیتزدایی، سیلیسی شدن، پیریتی شدن، سیمانی شدن و شکستگی، در مراحل مختلف دیاژنز دریایی، متئوریک، دفنی و تلوژنز نام برد. | ||
کلیدواژهها | ||
سازند فهلیان؛ میکرایتی شدن؛ دیاژنز دفنی؛ ریز رخساره؛ رو به باد؛ ماسهسنگهای آهکی | ||
مراجع | ||
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