Titlebook: Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a; Proceedings of the 1 Attila Çiner,San

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Distribution of Surface Sediments at the Bottom of Lake Ladogaof surface sediments at the bottom of Lake Ladoga using new methods. Based on the research results, a new map of the distribution of bottom sediments has been compiled, which can serve as a qualitative basis for monitoring the ecological situation in the lake.

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Sedimentology and Depositional Facies Architecture of the Cenomanian Ain Tobi Formation, Nafusah Escsion was deposited broadly on a shallow carbonate ramp setting. Five detailed sections were measured from the northeastern to the southwestern parts of the NE and logged using the standard logging technique. Sixty thin sections were examined and interpreted better to understand the vertical and late

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Distribution of Surface Sediments at the Bottom of Lake Ladogater quality in the lake. Therefore, it is necessary to study them. Researchers from the Institute of Limnology of RAS are looking at the distribution of surface sediments at the bottom of Lake Ladoga using new methods. Based on the research results, a new map of the distribution of bottom sediments

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Upper Pleistocene-Holocene Coastal Depositional Sediments of the Farwah Spit, NW Libyasitional system comprises salt marsh, tidal flat, lagoon, flood delta, and spits. Sedimentological analysis of outcrops, integrated with satellite image interpretation and comparison with equivalent deposits from neighbouring provinces, allows an understanding of the genesis and timing of the Holoce

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Facies, Sedimentology, and Characterization of the Depositional Environments of the Lower Liassic (Lnsidered a vast, shallow depression originating from an N-S to NE-SW half-graben structure. According to up-to-date analyses, the deposits in the MBEB basin can be subdivided into two major series: lower argillaceous-salt series attributed to the Triassic and Upper argillaceous-salt series attribute

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