Deformation Mechanisms and Microstructures Flashcards
microscale deformation mechanisms that occurs within individual mineral grains
Intracrystalline deformation
when the intracystalline deformation produces microstructure that affecting more than onebgrain such as grain boundary sliding or fracturing of mineral aggregates that is common in brittle deformation
Intercystalline deformation
strain expression of mechanical bending or kinking of the crystal lattice particularly at very low temepratures Pagioclase and calcite
Deformation twins
The process of forming deformation twins
mechanical twinning
This mineral exhibit a kind of deformation twin that involves simple shear along the twin plain where the kinked and unkinked part are mirror of one another about this plane occuring at a shear stress just above critical threshold of 10MPa.
This means, that it can deform by twinning at any level in the crust, and by surface as long the critical threshold is reached.
Calcite
True or False: The more defects in a crystal lattice wether deformed or not, the higher the stored energy.
True
Movement of vacancies
Diffusion
crystal deffects that represented by either vacancies or less i portsntly impurities in the form of extra atoms in the lattice but the interest to some, is the point defect reperesented by missing atoms
Point defect
a mobile line defect that contributes to intracrystalline deformation by a mechanism called slip ( movement of dislcation font within a plane)
Line defects/dislocation
is a mechanism involving migration of vacancies in crystallograpic in crystallograpic lattices
Diffusion or creep
is a diffusion of vacancies through crystal wherein strain rate is taken into consideration, the higher smaller the grains, the higher the strain rate. keep in mind that the strain rate is not high, however at some point, when reach a grain boundary, the vacancies will then dissappear.
Nabarro - Herring Creep
Because vacancies move toward sites of maximum stress, what does the final shape of the crystal acquire? during this process the crystal will gain regularity to become a regular crystal
fabric or strain
True or False: Volume diffusion requires a lot energy so that the migration rate is highly temperature dependent: high temperature high vibration in the lattice, which increase rate
True
is a migration of vacancies occurs at preferentially along grain boundaries. It is a bit less energy demanding than Nabarro-Herring Creep, and is more important in the formation of the plastic crust
Grain Boundary-Coble creep
bears similarity to Coble Creep and geometrically and mathematically it can be treated in the same way.
Pressure solution or wet diffusion