نویسندگان
1 استاد، گروه زمین‌شناسی دانشگاه لرستان، خرم‌آباد، ایران
2 گروه زمین‌شناسی، دانشگاه لرستان، خرم‌آباد، ایران
3 دانشجوی کارشناسی ارشد، چینه‌شناسی و فسیل‌شناسی، دانشگاه لرستان، خرم‌آباد، ایران
4 دانشجوی دکتری، رسوب‌شناسی و سنگ رسوبی، دانشگاه بوعلی‌سینا، همدان، ایران
چکیده
کلیدواژه‌ها
عنوان مقاله [English]
نویسندگان [English]
The Surgah Formation is a deep marine sedimentary sequence that extends only in the Lorestan zone and its margins. In order to study the stratigraphic and biostratigraphic characterises of this formation, the Falakolddin section in the High Zagros zone, adjacent to the northern part of the Lorestan zone, was selected. The thickness of the Surgah formation in this section is 80.80 meters and includes dark gray medium to thick argillaceous limestones and limestones, which has more clay content compared to other outcrops of the Surgah Formation. In the biostratigraphic studies of this formation, 18 species of 7 genera of planktonic foraminifera were identified, based on their distribution, four biological zones were introduced, which are: Helvetoglobotruncana helvetica total renge zone, Marginotruncanasigali-Dicarinella primitiva partial range zone, Dicarinella concavata interval zone and Dicarinella asymetrica total range zone . Based on the introduced biozones , the age of Surgah Formation in this section has been determined Middle Turonian -Late Santonian
کلیدواژه‌ها [English]
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