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What is Crocker Formation Field Observations about?
Field work was carried out at three stations to study the Crocker Formation. Station 1 contained thick sandstone beds that alternated with thin shale layers, displaying sedimentary structures like lamination and Liesegang rings. Station 2 featured an anticline fold with associated thrust fault. Station 3 contained a normal fault that cut through sandstone and shale beds. Cataclastic rocks and slickenfibers were observed near the fault zone, indicating the direction of movement.
- Author
- Imran Amin
- Language
- EN