Search Results - "Zuo, Mingtao"
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Constraints on the organic matter accumulation of Lower Cambrian Niutitang Shales in the middle Yangtze region, south China
Published in Lithosphere (01-03-2021)“…The lower Cambrian Niutitang shales, as one of target intervals with the greatest potential for shale gas exploration and development, have attracted much…”
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The influence of hydrocarbon generation on the sealing capability of mudstone caprock rich in organic matter
Published in Scientific reports (22-01-2024)“…To investigate the sealing capability of mudstone caprock during the evolution of organic matter (OM)-rich mudstone, a series of hydrous pyrolysis experiments…”
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Platform margin belt structure and sedimentation characteristics of Changxing Formation reefs on both sides of the Kaijiang-Liangping trough, eastern Sichuan Basin, China
Published in Open Geosciences (13-03-2024)“…This article discusses the types and characteristics of platform margin belts on both sides of the Kaijiang-Liangping trough in the Sichuan Basin during the…”
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Distribution and controlling factors of the oolitic shoal deposits in the sequence stratigraphic framework: a case study of the Lower Triassic Feixianguan Formation, eastern Sichuan Basin, China
Published in Carbonates and evaporites (01-03-2021)“…As one of the main reservoirs types in the Sichuan Basin, the granular shoal reservoirs of the Feixianguan Formation have great potential for oil and gas…”
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Controls of Distinct Mineral Compositions on Pore Structure in Over-Mature Shales: A Case Study of Lower Cambrian Niutitang Shales in South China
Published in Minerals (Basel) (01-01-2021)“…Investigating the impacts of rock composition on pore structure is of great significance to understand shale gas occurrence and gas accumulation mechanism…”
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Sedimentary facies, lithofacies paleogeography, and an evaluation of the Ordovician sequences in the Sichuan Basin, southwest China
Published in Marine and petroleum geology (01-03-2023)“…Ordovician strata in the Sichuan Basin occur in formations of varying thicknesses. Deposited in intracratonic and craton margin depressions of the Yangtze…”
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