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Biostratigraphy of the Ruteh Formation at Harijan section (Central Alborz) northern Iran using foraminifera and conodont

机译:伊朗北部有孔虫和牙形石在哈里扬剖面(中阿尔伯兹中部)Ruteh组的生物地层学

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摘要

In order to study the fossil contents of the Ruteh Formation for biostratigraphical purposes, the 200 meters thick section was sampled at Harijan section, Central Alborz. The sequence is mainly made up of limestone and shale's. The lower contact of the formation with Dorud Formation is disconform while the upper contact with under learing Dorud Formation is disconformable with overling Nesen Formation is as well as disconformable. Fifty four species belonging to 27 genera (foraminifera and conodonts) were identified and three biozones were differentiated. These are formation: 1- _Schubertella giraudi_- _Codonofusiella distincta_ Assemblage Zone, 2- _Cribrigenerina sumatruna_- _Langella ocarina_ Assemblage Zone, 3- _Sweetognathus whitei_ Biozone. Based on, these an age of Yackhtaschian - Murghabian is quoted to the formation.
机译:为了研究Ruteh组的化石成分以用于生物地层学目的,在Alborz中部的Harijan段取样了200米厚的断面。层序主要由石灰岩和页岩层组成。地层与Dorud地层的下部接触是不连续的,而下部淋溶Dorud地层的上部接触却可以与上覆的Nesen地层不分离。鉴定了属于27属的54种(有孔虫和牙形石),并区分了3个生物区。它们是形成物:1-吉氏舒伯特氏菌-明显的Codonofusiella-聚集区,2-中华鳞翅目-_Langella ocarina_聚集区,3- Sweetognathus whitei_生物区。基于此,引用了Yackhtaschian-Murghabian的年龄。

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