The Sedimentary Characteristics and Resource Potential of a Lacustrine Shallow-Water Delta on a Hanging-Wall Ramp in a Rift Basin: A Case Study from the Paleogene of the Raoyang Sag, Bohai Bay Basin, China

Lei Ye (), Xiaomin Zhu (), Nigel P. Mountney, Shuanghui Xie, Renhao Zhang and Luca Colombera
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Lei Ye: College of Geosciences, China University of Petroleum, Beijing 102249, China
Xiaomin Zhu: College of Geosciences, China University of Petroleum, Beijing 102249, China
Nigel P. Mountney: Sedimentology Research Group, School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK
Shuanghui Xie: College of Geosciences, China University of Petroleum, Beijing 102249, China
Renhao Zhang: China JIKAN Research Institute of Engineering Investigations and Design, Co., Ltd., Xi’an 710000, China
Luca Colombera: Department of Earth and Environmental Sciences, University of Pavia, Via Ferrata 1, 27100 Pavia, Italy

Sustainability, 2024, vol. 17, issue 1, 1-30

Abstract: The hanging-wall ramps of rift basins are prone to the accumulation of large sedimentary bodies and are potential areas for the presence of large subsurface geological reservoir volumes. This paper comprehensively utilizes data from sedimentology, seismic reflection, geochemistry, and palynology to study the paleotopography, water conditions, paleoclimate, and sediment supply of the fourth member (Mbr 4) of the Shahejie Formation in the Raoyang Sag of the Bohai Bay Basin, China. The sedimentary characteristics, evolution, and preserved stratigraphic architectures of shallow-water deltaic successions are analyzed. Multiple indicators—such as sporopollen, ostracoda, fossil algae, major elements, and trace elements—suggest that when Mbr 4 was deposited, the climate became progressively more humid, and the lake underwent deepening followed by shallowing. During rift expansion, the lake level began to rise with supplied sediment progressively filling available accommodation; sand delivery to the inner delta front was higher than in other parts of the delta, and highly active distributary channels formed a reticular drainage network on the delta plain, which was conducive to the formation of sandstone up-dip pinch-out traps. In the post-rift period, the lake water level dropped, and the rate and volume of sediment supply decreased, leading to the formation of a stable dendritic network of distributary channels. At channel mouths, sediments were easily reworked into sandsheets. The distribution of sandstone and mudstone volumes is characterized by up-dip pinch-out traps and sandstone lens traps. The network of channel body elements of the shallow-water deltaic successions is expected to act as an effective carbon dioxide storage reservoir. This study reveals the influence of multiple factors on the sedimentary characteristics, evolution, and internal network of shallow-water deltas at different stages of rift basin evolution. This knowledge helps improve resource utilization and the sustainable development of comparable subsurface successions.

Keywords: hanging-wall ramp; shallow-water delta; sedimentary environment; controlling factors; subsurface resource potential; Raoyang Sag (search for similar items in EconPapers)
JEL-codes: O13 Q Q0 Q2 Q3 Q5 Q56 (search for similar items in EconPapers)
Date: 2024
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