faults
High Pressures is the wrong answer. The correct asswer would be cooler tempeture.
This depends on the confining pressure, the temperature and the strain rate applied to the mineral. In general for minerals (and other materials), the lower the rate of strain, the more likely ductile or plastic creep deformation will occur. The higher the strain rate, the more likely brittle deformation is to occur. As the confining pressure increases, an objects shear strength will increase (this usually coincides with a greater depth of burial) and due to the earth's thermal gradient an increase in temperature. As the shear strength increases, brittle failure is less likely and the higher temperature means that plastic deformations or creep are more likely to occur.
Igneous rock
A fault is an example of brittle deformation which is defined as a loss of cohesion whereby a fracture or fractures propagate through the material.
ductile deformation
Faults are formed by brittle deformations and folds are formed by ductile deformation.
faults
Brittle
Brittle
High Pressures is the wrong answer. The correct asswer would be cooler tempeture.
it is when something breaks from its original shape and cannot return to its original form
In brittle fracture, no apparent plastic deformation takes place before fracture. In ductile fracture, extensive plastic deformation (necking) takes place before fracture.
This depends on the confining pressure, the temperature and the strain rate applied to the mineral. In general for minerals (and other materials), the lower the rate of strain, the more likely ductile or plastic creep deformation will occur. The higher the strain rate, the more likely brittle deformation is to occur. As the confining pressure increases, an objects shear strength will increase (this usually coincides with a greater depth of burial) and due to the earth's thermal gradient an increase in temperature. As the shear strength increases, brittle failure is less likely and the higher temperature means that plastic deformations or creep are more likely to occur.
Igneous rock
A fault is an example of brittle deformation which is defined as a loss of cohesion whereby a fracture or fractures propagate through the material.
Can deformation occur without metamorphism? (; sorry you should put the definitions in the description box when you're dealing with big words haha.