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Biostratigraphy and Lithostratigraphy of Pabdeh Formation Sediments (Middle Paleocene-Upper Eocene) in the Zagros Basin, Southwest Iran

机译:Pabdeh形成沉积物(中古)沉积物(中古)在ZAGROS盆地,西南伊朗西南部的生物数据和岩石岩

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摘要

The 530 thin sections from the Farashband region were investigated to study the Pabdeh Formation sediments in the Fars region. The 210 meters thick Pabdeh Formation is located in the Farashband fold section. The Pabdeh Formation's geology consists mostly of thin to medium-bedded limestone, argil-lite lime, shale and marl. The Pabdeh Formation's lower boundary is in disconformity with the Gurpi Formation (Campanian-Middle Maastrichtian), while its upper boundary is in conformity with the Asmari Formation (lower oligocene). The 14 speciesbelonging to 31 planktonic and benthic Foraminifera types and 5 planktonic Foraminifera biozones {Mor-zovella unicinata zone-Morzovella velascoensis Zone-Morzovella formosa Morzovella aragoensis Assemblage zone-Morzovella lehneri zone-Tur-borotalia cerroazulensis, Hantkenina Assemblage zone) were obtained in biostratigraphy analysis. The Pabdeh Formation's approximate age is upper Paleocene-Eocene according to identified fossilized content and biozones.
机译:研究了来自Farashband区域的530个薄切片,以研究波巴德地区的波巴德地区沉积物。 210米的Pabdeh形成位于Farashband折叠部分。 Pabdeh形成的地质主要由薄于中型石灰石,argil-lite石灰,页岩和马尔。 Pabdeh形成的较低边界是与Gurpi形成(Campanian-中间Maastrichtian)的令人讨厌的程度,而其上边界符合Asmari形成(下寡烯)。 在生物数据库中获得了14种彼此植物和5型浮游生物型和5型浮游生物的Foraminifera-Morzovella Morzovella-Morzovella Lehneri Zone-tur-Borotalian Cerroazulensis(汉氏菌·莫拉莫氏菌) 分析。 PabdeH形成的近似年龄是鉴定的化石含量和生物氮杂的群岛。

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