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Crust deformation

Home » Crust deformation
The three deformation mechanisms viscous, elastic, and brittle (a.k.a. plastic).

Deformation mechanisms

The three deformation mechanisms viscous, elastic, and brittle (a.k.a. plastic).

Spatial and temporal scales of common geodynamic processes, which occur over a wide range of time and length scales.

Geodynamic scales

Spatial and temporal scales of common geodynamic processes, which occur over a wide range of time and length scales.

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