首页> 外文期刊>Journal of the Geological Society of India >Microfacies Analysis and Cyclostratigraphy of the Upper Cretaceous-Lower Paleogene Succession of Bir Dakhl Section, North Eastern Desert, Egypt
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Microfacies Analysis and Cyclostratigraphy of the Upper Cretaceous-Lower Paleogene Succession of Bir Dakhl Section, North Eastern Desert, Egypt

机译:埃及东北沙漠Bir Dakhl剖面上白垩统-下古近纪演替的微相分析和旋回地层学

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摘要

The Bir Dakhl section which is located in the southern Galala plateau, north eastern desert was sampled for microfacies analysis of the upper Cretaceous-lower Paleogene succession. Microfacies analysis led to the recognition of eight mixed clastic-carbonate facies types (black shale lithofacies MF-1, pure shale lithofacies MF-2, sandy shale lithofacies MF-3, marly shale lithofacies MF-4, mudstone microfacies MF-5, foraminiferal wackestone microfacies MF-6, bioclastic wackestone microfacies MF-7, and bioclastic packstone microfacies MF-8) of the studied interval. These microfacies can be grouped into three depositional environments: inner, middle and outer ramp. The interpreted depositional environments have been suggested to range from neritic to middle bathyal (similar to 700 m). Based on cyclostratigraphy, five deepening upward cycles and three shallowing upward cycles have been differentiated in Bir Dakhl section.
机译:对位于东北沙漠南部加拉拉高原的Bir Dakhl断面进行了采样,以对白垩纪-下古近纪演替进行微相分析。微相分析导致了八种混合碎屑碳酸盐相类型的识别(黑色页岩岩相MF-1,纯页岩岩相MF-2,砂质页岩岩相MF-3,马利页岩岩相MF-4,泥岩微相MF-5,有孔虫沃克石微相MF-6,生物碎屑沃克石微相MF-7和生物碎屑堆积石微相MF-8)。这些微相可分为三个沉积环境:内部,中部和外部斜坡。已提出解释性沉积环境的范围为从浅碱性到中性深海(约700 m)。根据旋回地层学,在Bir Dakhl剖面上已区分出五个加深的向上旋回和三个浅化的向上旋回。

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