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16 Pliegues Sinsedimentarios, Fac. Ing., UNAM

16 Pliegues Sinsedimentarios, Fac. Ing., UNAM

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Sediments that have not yet consolidated often give rise to folds when they are situated on a gentle slope and experience some form of sliding. The possible causes of the sliding include seismic shocks, water oversaturation, freezing and thawing, erosion and loading of a slope.

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