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This study aims to identify the sedimentary model and facies evolution of K-Successions sandstones in the H21 Area of Huizhou Depression, Pearl River Mouth Basin, South China Sea. The researchers analyzed lithological characteristics, lithofacies, sedimentary sequences, and seismic attributes to determine the sandstones were deposited in a nearshore sand bar-sheet system, rather than previous models of fluvial-dominated or tide-dominated systems. They identified seven lithofacies and divided the delta evolu

Author

Abassyacoubou

Language

EN