Geochemical Characterization and Paleo-Burial History Modeling of Unconventional Resources: A Case Study from the Ordovician Wulalike Formation (O<sub>2</sub>w) in the West Margin of the Ordos Basin (North China). [PDF]
Huang Z +10 more
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Petrology of the Sandstone-Type Uranium Target Layer and Its Uranium Existence Form in the Telaaobao Mineral Area, Ordos Basin. [PDF]
Sun D +6 more
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Genesis and Accumulation Modes of Coalbed Methane at the Eastern Margin of Ordos Basin, China: Evidence from Its Geochemistry. [PDF]
Li Z, Chen S, Tang D, Zhi Y.
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Pore-throat structure, fractal characteristics and permeability prediction of tight sandstone: the Yanchang Formation, Southeast Ordos Basin. [PDF]
Zhang H, Guo L, Wu Z, Ma J.
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Effect of Depositional Environment on the Occurrence of 17α(H)-Diahopanes in Triassic Lacustrine Sediments from the Ordos Basin, NW China. [PDF]
Shi B, Liang Q, Liu E, Ai X, Wang R.
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Gas-Water Distribution and Gas Reservoirs Accumulation Properties of Upper Paleozoic Sequence in the Western Yishan Slope, Ordos Basin, NW China. [PDF]
Yang Z, Zhou J, Chen J, Cheng W, Jing S.
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Mineralogy and Geochemistry of Rare Earth Elements in Carboniferous-Permian Coals at the Eastern Margin of the Ordos Basin. [PDF]
Wen L +6 more
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Upper Paleozoic petroleum system, Ordos Basin, China
Marine and Petroleum Geology, 2005Abstract The Ordos Basin is a typical lapped basin, including three sequences of strata: early Paleozoic, late Paleozoic and Mesozoic, with a total thickness of 4000–6000 m. Impermeable sealing beds are well developed at the top and base of the upper Paleozoic sequence, separating it from the Mesozoic and the lower Paleozoic strata to form an ...
X.M. Xiao +4 more
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Dynamic origin of anomalous subsidence of Jurassic Ordos basin
2022<p>The Jurassic Ordos basin is generally considered an intracontinental basin characterized by rapid subsidence rate along western margin and slow subsidence rate within basin interior. However, the formation mechanism of Ordos basin was not yet well understood. Flexural backstripping of stratigraphic record spanning from 174-153Ma, along
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