2020
DOI: 10.1016/j.petrol.2020.107947
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Siliciclastic depositional model within a subsurface coastal parasequence based on barriers and baffles – An application to the Donghe Sandstone Member in the Hudson Oilfield, Tarim Basin, NW China

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Cited by 8 publications
(5 citation statements)
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“…4b). Previous studies (Sun et al, 2020;Lei et al, 2019Lei et al, , 2021Li et al, , 2023 suggest that these sandstones deposits originate from wave-dominated shoreface environments. In the Donghetang area, the Donghe sandstones have a thickness of approximately 250 meters, with a buried depth ranging from 5700 to 6000 meters.…”
Section: Marine Sandstonesmentioning
confidence: 82%
“…4b). Previous studies (Sun et al, 2020;Lei et al, 2019Lei et al, , 2021Li et al, , 2023 suggest that these sandstones deposits originate from wave-dominated shoreface environments. In the Donghetang area, the Donghe sandstones have a thickness of approximately 250 meters, with a buried depth ranging from 5700 to 6000 meters.…”
Section: Marine Sandstonesmentioning
confidence: 82%
“…The Donghe sandstone member is a typical marine clastic reservoir rich in oil and gas in China. 33 Limited by the “three highs” of high temperature, high salinity, and high pressure, appropriate injection and production systems need to be formulated during the development. After tracking and analyzing the oil and gas production in the process of gas injection and oil displacement, it is found that the oil and gas production of gas injection and oil displacement technology is directly related to the injection volume of gas injection wells, water injection wells, and the flowing bottom-hole pressure of production wells.…”
Section: Resultsmentioning
confidence: 99%
“…The Donghe sandstone member is a typical marine clastic reservoir rich in oil and gas in China. 33 Limited by the "three highs" of high temperature, high salinity, and high pressure, appropriate injection and production systems need to be formulated during the development.…”
Section: Resultsmentioning
confidence: 99%
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“…As the compaction continues, the shale enters the middle diagenetic stage. The formation temperature and pressure increase, and the montmorillonite continues to dehydrate, resulting in interlayer collapse [56]. Organic matter generates hydrocarbons in large quantities and produces organic acid, resulting in acidic pore fluid [57].…”
Section: Diagenetic Evolution Sequence Of Shalementioning
confidence: 99%