2023
DOI: 10.1016/j.engeos.2022.07.004
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Exploration progress of the Paleogene in Jiyang Depression, Bohai Bay Basin

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Cited by 13 publications
(11 citation statements)
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“…The grain core is dirty and the color of the ring edge is usually bright. If the crystal shape is good, the bright edge fog center structure is obvious (Briais et al, 1993;Budd, 1997;Hong et al, 2004;Ma et al, 2023).…”
Section: Petrological Characteristicsmentioning
confidence: 99%
“…The grain core is dirty and the color of the ring edge is usually bright. If the crystal shape is good, the bright edge fog center structure is obvious (Briais et al, 1993;Budd, 1997;Hong et al, 2004;Ma et al, 2023).…”
Section: Petrological Characteristicsmentioning
confidence: 99%
“…[9][10][11][12][13][14] In recent years, there has been an increasing focus on beach-bar sedimentary systems for exploring stratigraphic traps in various basins in eastern China. [15][16][17][18] Herein, beach bar sandstones are particular shallowwater deposits, with low mud content and good petrophysical properties. Most importantly, beach bar sandstones are generally covered by a thick layer of mudstone which creates a proper reservoir-cap combination, to trap hydrocarbons.…”
Section: Introductionmentioning
confidence: 99%
“…Overall, beach bar sand bodies have favorable conditions to become a target for hydrocarbon exploration activities due to their proximity to the oil source, good reservoir properties and well‐configuration of source, reservoir and cap rock, which is conducive to large‐scale oil and gas enrichment 9‐14 . In recent years, there has been an increasing focus on beach‐bar sedimentary systems for exploring stratigraphic traps in various basins in eastern China 15‐18 . Herein, beach bar sandstones are particular shallow‐water deposits, with low mud content and good petrophysical properties.…”
Section: Introductionmentioning
confidence: 99%
“…Bonan sub-sag is a secondary sag in the middle of Zhanhua Sag of Jiyang depression, and the Bonan sub-sag is steep in the north-east and slow in the south-west of the faulted basin (Dong, 1993). The Bonan sub-sag is separated by Chengdong Fault and borders with Chengzikou High in the north, separated by Gudong Fault and lies on the west of Gubei Sub-sag, separated by Yidong Fault and is next to Yihezhuang High in the west, and borders with the Chenjiazhuang High in the south (Hu., 2013;He et al, 2016;Ma et al, 2022). The depositional environment of the First Member of Shahejie Formation (Es1) is mainly a deep to semi-deep lake, with the development of a set of thick mud shale with an average thickness of more than 50 m, and forming a source of insufficient supply of brackish to semi-brackish water in a deep to semi-deep lake depositional environment (Li et al, 2018;Song et al, 2022;Zhang et al, 2012).…”
Section: Introductionmentioning
confidence: 99%