water Article Determination of Paleocurrent Directions Based on Well Logging Technology Aiming at the Lower Third Member of the Shahejie Formation in the Chezhen Depression and Its Implications Yangjun Gao 1,2, Furong Li 2,3, Shilong Shi 2 and Ye Chen 1,4,* 1 School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
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[email protected] (S.S.) 3 Faculty of Land and Resources Engineering, Kunming University of Science and Technology, Kunming 650093, China 4 School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China * Correspondence:
[email protected] Abstract: The Bohai Bay basin, mainly formed in the Cenozoic, is an important storehouse of groundwater in the North China Plain. The sedimentary deposits transported by paleocurrents often provided favorable conditions for the enrichment of modern liquid reservoirs. However, due to limited seismic and well logging data, studies focused on the macroscopic directions of paleocurrents L are scarce. In this study, we obtained a series of well logging data for the sedimentary layers of Es3 Formation in the Chezhen depression. The results indicate the sources of paleocurrents from the northeast, northwest, and west to a center of subsidence in the northern Chezhen depression at that Citation: Gao, Y.; Li, F.; Shi, S.; time. Based on the well testing data, the physical properties of the layers from Es L Formation in Chen, Y. Determination of 3 Paleocurrent Directions Based on this region were generally poor, but two abnormal overpressure zones were found at 3700–3800 m Well Logging Technology Aiming at and 4100–4300 m deep intervals, suggesting potential high-quality underground liquid reservoirs.