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

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Post-oligocene Tectono-Eustatic Fluctuations and Their Influence on the Stratigraphy of Eastern Arabthe low-lying region between the Al-Hajar Mountains and the coast of the Gulf of Oman. The group is divisible into three tectonostratigraphic successions represented by three formations: Sultan Qaboos University (SQU), Suwadi, and Barzaman, in ascending order. The SQU Formation consists of conglomer

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Establishment of Geological Age Under the Constraints of Astronomical Cycles in Dongying Saggeological age has always been a scientific problem. Astronomical cycle analysis is an effective method developed for high-resolution stratigraphic research in recent years. We apply this method to improve the accuracy of the stratigraphic age of the ash-deficient section of lacustrine fine-grained

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Spectral Gamma-Ray Variability Within Carbonate Lithofacies: An Example from the Early Triassic Lowery facies. Spectral gamma-ray is widely used in depositional facies and sequence stratigraphic analysis. Here, spectral gamma-ray U, Th, and K measurements from two logged sections of the Early Triassic Lower Mahil Formation (Upper Khuff-equivalent, KS1) of Al Jabal Al-Akhdar (Saiq Plateau and Wadi

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Early Pliocene Benthic Foraminifera of the Southeastern Coast of Cap Bon Peninsula (Northern Tunisia of the Jrêba section (Nabeul region, southeastern coast of the Cap Peninsula, Tunisia). A diversified micro-faunistic content was documented, consisting of 36 species of benthic foraminiferal belonging to 26?genera and 21 families. Among these species: .,?.?., .,?C.,?. These species are ecologicall

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The Geochemistry of Biotite from TTG Batholiths and A-type Complexes (Silet Region, Hoggar, Algeria)) batholiths and four A-type complexes. All of them are exposed in the central part of the Silet terrane (western Hoggar, Algeria) and crosscut Pharusian volcano-sedimentary series. According to Nd isotope values, the rocks are geographically arranged in two narrow N-S oriented bands separated by th