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Typical disequilibrium compaction caused overpressure of Paleocene Dongying Formation in northwest Liaodongwan Depression, Bohai Bay Basin, China

Marine GeologyBasin EvolutionEngineeringPaleocene Dongying FormationGeographyTectonic EvolutionBohai Bay BasinGeochronologyPaleoecologyTypical Disequilibrium CompactionEarth ScienceSocial SciencesTectonics