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This research reviews and critiques the relationships between normal fault displacement (D) and length (L), highlighting the variability influenced by geological factors such as fault size, maturity, and host rock lithology. The authors present a new database of 4059 normal faults, revealing a scaling law of D = 0.3L^0.92, which can aid in predicting fault dimensions and understanding fault growth dynamics. This comprehensive study provides an open-access resource for the structural geology community to ana

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convenienceo5
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