cataclastic flowの例文
- Five main mechanisms are recognized; cataclastic flow, dislocation creep, recrystallization, diffusive mass transfer and grain-boundary sliding.
- Cataclastic flow is generally instable and will terminate by the localization of deformation into slip on fault planes, where fault propagation can allow cataclasis to migrate into nearby areas of the rock volume.
- After those two initial deformations, several other types of secondary brittle deformation can be observed, such as " frictional sliding " or " cataclastic flow " on reactivated joints or faults.
- Cataclastic flow usually occurs at diagenetic to low-grade metamorphic conditions, however this depends on the mineralogy of the material and the extent of pore fluid pressure, as high fluid pressure will promote cataclastic flow in any metamorphic environment.
- Cataclastic flow usually occurs at diagenetic to low-grade metamorphic conditions, however this depends on the mineralogy of the material and the extent of pore fluid pressure, as high fluid pressure will promote cataclastic flow in any metamorphic environment.
