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This study introduces a modified elliptic Fourier analysis method to quantitatively analyze the shape differences of mud clasts in hybrid event beds, revealing significant variations linked to depositional facies. The research demonstrates that traditional shape analysis methods are inadequate for capturing the complex shapes of mud clasts, while the new method effectively visualizes these differences and their implications for sediment transport processes. Results from the Otadai Formation in Japan indicat

Author

harisma

Language

EN