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首页> 外文期刊>Neues Jahrbuch fur Geologie und Palaontologie. Abhandlungen >Foraminifera and sequence stratigraphy of Burdigalian – Serravallian successions on the eastern side of the Gulf of Suez, southwestern Sinai, Egypt
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Foraminifera and sequence stratigraphy of Burdigalian – Serravallian successions on the eastern side of the Gulf of Suez, southwestern Sinai, Egypt

机译:埃及西奈西南部苏伊士湾东侧的布尔迪加利-塞拉瓦利亚演替的有孔虫和层序地层

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摘要

Stratigraphical studies of Miocene exposures on the eastern side of the Gulf of Suez (Wadi Gharandal, Wadi Baba and Wadi Feiran) reveals conspicuous vertical and lateral facies variations due to syngenetic tectonic activity related to rifting. Studied samples include 88 species of foraminifera (39 planktonics and 49 benthonics). Six planktonic biozones (M2-M7) were distinguished. The sequence statigraphical investigation of the Burdigalian to Serravallian succession reveals six thirdorder depositional sequences, bounded by physical unconformity surfaces reflecting phases of subaerial exposure, deposition of alluvial fans, polymictic conglomerates, evaporites and the presence of a faunal break, which could be correlated within and outside Egypt. These sequence boundaries are primarily related to regional tectonism associated with rifting or related to eustatic sea-level fluctuations.
机译:苏伊士湾东侧(Wadi Gharandal,Wadi Baba和Wadi Feiran)中新世暴露的地层学研究表明,与裂谷有关的同生构造活动导致明显的垂直和横向相变。研究样本包括有孔虫88种(39种浮游生物和49种底栖鱼类)。区分了六个浮游生物区(M2-M7)。从布尔迪加利到塞拉瓦利亚演替的层序地层学研究揭示了六个三阶沉积层序,其边界是物理不整合面,反映了空中暴露,冲积扇沉积,多聚砾岩,蒸发岩和动物区系破裂的相,这可能与内部和内部相关。在埃及以外。这些层序边界主要与裂谷作用有关的区域构造或与海平面波动有关。

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