نشریه علوم زمین خوارزمی

نشریه علوم زمین خوارزمی

چینه‌نگاری زیستی سازند گورپی بر مبنای نانوفسیل‌های آهکی در برش تاقدیس کوه سفید، زون ساختاری ایذه

نویسنده
دانشگاه بین المللی امام خمینی (ره)، دانشکدۀ فنی
چکیده
در پژوهش حاضر 190 متر از رسوبات سازند گورپی در تاقدیس کوه سفید از نقطه نظر نانوفسیل‌های آهکی بررسی شد. در این برش سازند گورپی اساسا از شیل، مارن و سنگ آهک رسی تشکیل شده است. بررسی نانوفسیل­های آهکی در این قسمت منجر به تشخیص 21 جنس و 41 گونه شد. بر اساس پراکندگی گونه­های شاخص نانوفسیلی، زیست­زون­های CC25-CC16 تشخیص داده شد که این زون­ها با زیست زون­های UC12 تاUC20aTP مطابقت دارد. بر اساس زون‌های زیستی ­بهدست آمده، بازۀ زمانی سازند گورپی در این برش از سانتونین میانی/پسین تا اوایل ماسترشتین پسین است. بررسی در برش تاقدیس کوه سفید نشان می­دهد رسوب‌گذاری سازند گورپی در سانتونین میانی/پسین آغاز شده و تا اوایل ماسترشتین پسین ادامه داشته است.
کلیدواژه‌ها

عنوان مقاله English

Biostratigraphy of the Gurpi Formation based on Calcareous Nannofossil in the Kouh-e Sefid Anticline Section, Izeh Structural Zone

نویسنده English

Saeedeh Senemari
Imam Khomeini International University
چکیده English



The Gurpi Formation with a thickness of 190 m at the Kouh-e Sefid anticline is investigated based on the calcareous nannofossils. In this section, Gurpi Formation is mainly consists of shale, marls and argillaceous limestones. As a result of this study, 21 genera and 41 species of calcareous nannofossil have been recognized. Based on distribution of index species calcareous nannofossils CC16-CC25 biozones have been recognized, that is corresponding to UC12-UC20aTP. According to the identified biozones, the age of the Gurpi Formation in this section is middle/late Santonian to early late Maastrichtian. This study in the Kouh-e Sefid anticline shows that the sedimentation of Gurpi Formation started at the middle/late Santonian and continued to the early late Maastrichtian

کلیدواژه‌ها English

 Biozones
Zagros
Cretaceous
Kouh-e Sefid
Nannofossils
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