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This document discusses several methods for determining fault movement from geological structures: 1. The relationship between fault movement and associated structures like gash fractures, shear fractures, and microfolds can indicate the fault movement. 2. The angle between associated structures and the fault can provide information about the magnitude of fault movement. 3. Fracture patterns in rock, like grain boundaries and pinnate fractures, can be used to determine the direction of fault slip. 4.

Author

Annisa Puspa

Language

EN