2021
DOI: 10.1007/s11802-021-4569-7
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Relationship Between Paleogene Reservoir Densification and Hydrocarbon Accumulation in the Xihu Depression

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(2 citation statements)
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“…It features a petroleum-generating interval in the lower part of the Pinghu Formation and Baoshi Formation, reservoir-seal combinations of interbedded sandstones and mudstones in the middle part, and the migration of oil and gas along faults and stepped passages formed by the sandbodies. The accumulation processes include two stages: the pre-5 Ma Longjing movement and the post-5 Ma Longjing movement [31][32][33][34][35][36][37][38] (Figure 4). The Baoyunting nose is generally located in the accommodation zone margin (also known as the transition zone) between the gentle Wuyunting slope in the north and the steep Tuanjieting slope in the south (Figure 2).…”
Section: Regional Geological Backgroundmentioning
confidence: 99%
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“…It features a petroleum-generating interval in the lower part of the Pinghu Formation and Baoshi Formation, reservoir-seal combinations of interbedded sandstones and mudstones in the middle part, and the migration of oil and gas along faults and stepped passages formed by the sandbodies. The accumulation processes include two stages: the pre-5 Ma Longjing movement and the post-5 Ma Longjing movement [31][32][33][34][35][36][37][38] (Figure 4). The Baoyunting nose is generally located in the accommodation zone margin (also known as the transition zone) between the gentle Wuyunting slope in the north and the steep Tuanjieting slope in the south (Figure 2).…”
Section: Regional Geological Backgroundmentioning
confidence: 99%
“…It features a petroleum-generating interval in the lower part of the Pinghu Formation and Baoshi Formation, reservoir-seal combinations of interbedded sandstones and mudstones in the middle part, and the migration of oil and gas along faults and stepped passages formed by the sandbodies. The accumulation processes include two stages: the pre-5 Ma Longjing movement and the post-5 Ma Longjing movement [31][32][33][34][35][36][37][38] (Figure 4). According to the combined profile and plane morphology of the faults, as well as the stratigraphic occurrence, the Baoyunting area can be divided into five secondary structural units: fault fan (FF), high-belt east-dipping fault slope (HFS), fault saddle (FS), fault horst (FH), and low-belt east-dipping fault slope (LFS) (Figure 3).…”
Section: Regional Geological Backgroundmentioning
confidence: 99%