آمونیت های سازند کژدمی در کوه سیوند، برش شول، شمال شیراز در حوضه زاگرس، کاربرد دیرینه بوم شناسی
محورهای موضوعی : چینه شناسیناصر رئیس السادات 1 , مهناز پروانه نژاد شیرازی 2
1 - دانشگاه بیرجند
2 - دانشگاه پیام نور
کلید واژه: آمونیت, آلبین, سازند کژدمی, دیرینه بوم شناسی, حوضه زاگرس,
چکیده مقاله :
سازند کژدمی در حوضه زاگرس گسترش داشته و دارای دو رخساره کم عمق و عمیق می باشد. برش مورد مطالعه در شمال شیراز در کوه سیوند در نزدیکی روستا شول قرار داد. برش مورد مطالعه با ضخامت 210 متر شامل سنگ آهک، سنگ آهک مارنی و سنگ آهک های لایه نازک می باشد. چهار گونه Knemiceras persicum Collignon, 1981, Knemiceras aff. persicum Collignon, 1981, Knemiceras aff. iraniense Collignon, 1981, Knemiceras dubertreti Basse, 1940, مورد شناسایی قرار گرفتند و توصیف شدند.
بررسی آمونیت های سازند کژدمی نشان می دهد، گروههای شکلی متفاوت در این سازند پراکنده هستند.. به طوریکه در غرب حوضه و فروافتادگی دزفول آمونیت های اسفروکونیک با تزئینات کم پراکندگی بیشتر دارد که نشانه دهنده عمق بیشتر است، در حالیکه در نواحی استان فارس و بوشهر آمونیت های با تزئینات بیشتر که نشانه دهنده عمق کمتر حوضه است، گسترش دارند.در برش شول نیز مجموعه آمونیتی نیز عمق کم را پیشنهاد می کند که این امر با حضور فرامینیفرهای بنتیک پشتیبانی می شود.
Kazhdami Formation is spread in Zagros basin and has two facies, shallow and deep. The studied section was located in the north of Shiraz near the village of Shul. The lithology of the measured section with 210 meters thickness including limestone, marly limestone and thin layer limestone. Four species Knemiceras persicum Collignon, 1981, Knemiceras aff. persicum Collignon, 1981, Knemiceras aff. iraniense Collignon, 1981, Knemiceras dubertreti Basse, 1940, were identified and described.
Different ammonite morphogroups are distributed in the Kazhdumi Formation. spheroconic ammonites with low ornamentation, mostly ribs, usually live at sea level and away from the coast spread in the west of basin and Dezful depression. Plano-spiral ammonites with coarse ornaments were poor swimmers and indicate a shallow depth basin.
In the Shul section the ammonite assemblage with coarse ornamentation suggest a shallow environment that is supported with presence of benthic foraminifera assemblage.
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