Titlebook: Recent Research on Sedimentology, Stratigraphy, Paleontology, Geochemistry, Volcanology, Tectonics, ; Proceedings of the 2 Attila Çiner,Ste

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Middle to Late Cambrian Marine Transgression Depositional System of the Peri-Gondwana Terranes: An E Bashair Formation is an important deep hydrocarbon-producing subsurface reservoir in the interior Oman Salt Basin. The current outcrop-based stratigraphic and facies analysis of the Al Bashair Formation in the Huqf region has shed new insights to better understand the spatial and temporal distribut

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ICLE

Lithofacies Associations and Depositional System of the Muti Formation, Oman Mountainsd basin is a major hydrocarbon-producing basin with great future exploration potential. A few studies were published in the early 1990; however, no detailed work on the sediments of the Muti Formation has been done since then. The closure and compression of the southeast margin of the Tethys Ocean d

rods366

Middle Cambrian Marine Transgressive-Regressive Depositional System of the Peri-Gondwana Terranes: Aral Oman. The formation is among the complex, deep tight gas reservoirs in the interior Oman Salt Basin. The formation has been previously interpreted as deposits of interconnected ephemeral playa lakes, aeolian dunes, and wet and dry sabkha environments. Lithologic reevaluation of the rocks in the

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Late Cambrian-Early Ordovician Hybrid-Energy Deltaic System of the Peri-Gondwana Terranes: An Exampl is a complex, deep, tight gas reservoir in Oman’s interior Salt Basin and has been previously interpreted as braid delta deposits. This study illustrates a detailed outcrop-based stratigraphic and facies analysis of the Barik formation in the Huqf region. It offers new insights into the spatial and

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Depositional Facies and Sea-Level Variation of the Cryogenian Glacial System: An Example from the Ouhydrocarbon target in Oman, its spatial and temporal depositional facies distribution is still poorly understood. This study aims to build on previous outcrop studies and develop a depositional model based on detailed sedimentological logging of the well-exposed Fiq Formation in the Jabal Akhdar are

Foam-Cells

Sedimentary and Stratigraphic Description of the Castellón B Borehole Cores (Offshore Western Meditentary succession from eastern Iberia. Six stratigraphic units were recognized: (i) a Black Sandstone Unit, (ii) a Red Beds Unit, (iii) the Alcanar Conglomerates, (iv) the Tarraco “Shale,” (v) the Amposta Limestone, also known as “Amposta Chalk,” and (vi) the San Carlos Group. The Black Sandstone Uni

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New Carbon-Isotope, Conodont, and Magnetostratigraphic Data from the Key Kulyumbe River Section (NW brian-Ordovician (Cm-O) successions on the entire Siberian Platform. It is a key section for regional correlation of the Furongian-lower Ordovician interval in Siberia. However, the exact position of the Cm-O boundary as well as the boundaries of the global Ordovician stages in the section is still