distortion in a rock
deformation
transformation from an initial to a final geometry
geometric analysis
rigid body deformation
translation, rotation
non-rigid body deformation
distortion, dilation
deformation, change in volume
dilation
deformation, change in shape
distortion
relates in terms of displacement vectors in a displacement field
kinematic analysis
mechanics of materials with smoothly varying properties
continuum mechanics
processes that deform rocks at microscopic scales
microstructures
6 factors to deformation
3 groups of deformation mechanisms
brittle deformation, brittle flow, plastic flow
microscopic to submicroscopic cracks
microcracks
microcracks within a single grain, along a cleavage plane
intragranular microcracks
what causes intragranular microcracks
fracture strength of the grain lower than that of the boundaries
microcracks along grain boundaries
intergranular microcracks
what causes intergranular microcracks
boundaries being easier to crack
microcracks along adjacent grains and mutual grain boundaries
transgranular microcracks
what causes transgranular microcracks
strong grain boundaries and aligned cleavage planes
brittle fracturing and granulation
cataclasis
where is cataclasis common
shallow fault zones
repetition of crystal grains
mechanical twinning
where is mechanical twinning most common
plagioclase and calcite
more defects equals
more stored energy
migration of vacancies in lattices
diffusion creep