2019
DOI: 10.1016/s1876-3804(19)60251-x
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Trend judgment of abandoned channels and fine architecture characterization in meandering river reservoirs: A case study of Neogene Minhuazhen Formation NmIII2 layer in Shijiutuo bulge, Chengning uplift, Bohai Bay Basin, East China

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Cited by 5 publications
(3 citation statements)
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“…Its main characteristics are that the sand body is continuous, and mudstone or impermeable layer is developed on both the upper and lower parts of the sand body. Although some single sand bodies are connected with adjacent layers due to no interlayer, their internal fluid still constitutes an independent reservoir [1][2][3][4][5][6][7][8][9][10]. The chief geological factors affecting the distribution of remaining oil include sedimentary microfacies and the con-figuration relationship of the single sand body, reservoir lithology, physical properties, and heterogeneous characteristics.…”
Section: Introductionmentioning
confidence: 99%
“…Its main characteristics are that the sand body is continuous, and mudstone or impermeable layer is developed on both the upper and lower parts of the sand body. Although some single sand bodies are connected with adjacent layers due to no interlayer, their internal fluid still constitutes an independent reservoir [1][2][3][4][5][6][7][8][9][10]. The chief geological factors affecting the distribution of remaining oil include sedimentary microfacies and the con-figuration relationship of the single sand body, reservoir lithology, physical properties, and heterogeneous characteristics.…”
Section: Introductionmentioning
confidence: 99%
“…With the breakthrough in oilfield development and architectural structure theory, scholars have studied various types of sand body architecture, outcrop measurements, modern sediment systems, underground sand bodies, and reservoir modeling [2], of which the meandering river point bar sand body is the most extensively studied ( [1,[3][4][5][6]; Ji et al 2012; [7][8][9]). It is widely believed that a large amount of remnant oil can exist in the upper part of a point bar sand body due to the shielding of the interlayers of lateral deposits, whereas little or no remnant oil exist at the bottom due to the erosion of the lateral accretion [10][11][12][13][14][15].…”
Section: Introductionmentioning
confidence: 99%
“…(a) Plane view of the channel patterns in the PI2 layer. (b) Vertical profile of the channel in the PI2 layer 8. Geofluids the channel, and numerous parameters increase significantly in a similar way to the other flow units, which have obvious differences, thereby reflecting the characteristics of high flow velocity.…”
mentioning
confidence: 98%