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- W4200440903 abstract "The Ordos Basin, situated in the western part of the North China Block, has a long history that started in the Mesoproterozoic and extends to the Quaternary. It started as a marine basin, but was transformed into an intracratonic (largely lacustrine) basin when plates had collided during the Triassic. During the Carboniferous and Permian, but also during the Jurassic, huge coal deposits were formed. These are exploited in hundreds of coal mines but also resulted in several economically exploitable gas fields. The Triassic and the Jurassic contain large oil fields, particularly in the deposits of lacustrine deltas, but increasing interest has grown in tight oil and gas reservoirs that consist of fine-grained, deep-lacustrine deposits (mainly formed by turbidites and hyperpycnites extending from the front of the deltas to the deep center of the lake). The paleogeographical development of the Mesozoic lake is detailed." @default.
- W4200440903 created "2021-12-31" @default.
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- W4200440903 date "2022-01-01" @default.
- W4200440903 modified "2023-09-26" @default.
- W4200440903 title "Sedimentary and tectonic development of the Ordos Basin and its hydrocarbon potential" @default.
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- W4200440903 doi "https://doi.org/10.1016/b978-0-323-85264-7.00026-6" @default.
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