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• W4386276341 abstract "Upper Cretaceous sedimentary rocks are among the most important hydrocarbon reservoirs in the Persian Gulf. They contain significant information on the tectono-sedimentary evolution of the southern NeoTethys margin. This study focuses on the depositional facies and environments, paleontological content, relative ages, and sequence stratigraphy of these successions in the eastern Persian Gulf. Microfacies analysis indicate that the Cenomanian carbonates, Khatiyah and Mishrif members, were deposited on deep to shallow settings of a ramp-like carbonate platform, respectively. The sea-level drop and tectonic uplift formed a major paleoexposure surface at the top of the Mishrif Member. The Laffan Formation was deposited within the lacustrine setting, during the lowstand and early transgression of sea-level. Restoration of carbonate platform has resulted in the deposition of the Ilam carbonates. Biostratigraphic studies indicate the early Cenomanian age for the Khatiyah Member (biozone #23 and biofacies #26), a middle to late Cenomanian age for the Mishrif Member (biozone #22 and biofacies #24), a Coniacian age for the Laffan Formation (biozone #30A), and a Santonian age for the Ilam Formation (biozones # 30 and #31). Two third-order and five fourth-order depositional sequences were differentiated. Pelagic facies of the Khatiyah Member formed the TST, and neritic facies of the Mishrif Member formed the RST of Cenomanian sequence. The Laffan shale corresponds to the early TST, the basal part of the Ilam Formation to the late TST, and the upper part of the Ilam Formation to the RST of Coniacian–Santonian sequence. Identified sequences are well-correlated across the Persian Gulf." @default.
• W4386276341 created "2023-08-31" @default.
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• W4386276341 date "2023-01-01" @default.
• W4386276341 modified "2023-09-30" @default.
• W4386276341 title "Paleoenvironmental reconstruction, bio- and sequence stratigraphy of Upper Cretaceous (Cenomanian–Santonian) strata in the Persian Gulf, Iran" @default.
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• W4386276341 doi "https://doi.org/10.1016/bs.sats.2023.08.003" @default.
• W4386276341 hasPublicationYear "2023" @default.
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