Structural Geology L03 Flashcards
define pressure and stress.
pressure - force acting per unit area - does not have direction/vectors.
stress - amount of force exerted per unit area experienced
by a material (rock) - has direction/vector
Explain body forces and surface forces.
Body Forces
* Act throughout the volume of the solid
and directly proportional to its volume or
mass.
* Depends on the densities; while densities
itself depends on pressure.
Surface Forces
* Act only on the surface area bounding
a volume and arise from the
interatomic stresses exerted from one
side of the surface to the other.
* Increase linearly with depth known as
lithospheric stress/pressure.
differentiate normal stress and shear stress.
- stress vector oriented perpendicular to a
surface is called the normal stress on that
surface - stress vector that acts parallel to a surface
is referred to as the shear stress.
Explain principle stress direction.
Slide no 7
Types of stress in lithosphere.
- Residual stress
- lithostatic stress
- Tectonic stress
- Deviatoric stress
what is residual stress.
- Stress can be locked in and preserved after the external
force or stress field has been changed or removed - elastic strain remains after the external stress field is
removed.
for example,
– metamorphic transformations that involve volumetric
changes,
– intrusions where magma cooling sets up stresses that are locked into the crust,
– changes in temperature and/or pressure, or
– past tectonic episodes
What is tectonic stress.
stress related to plate movements and plate tectonics.
what is Anderson’s classification on tectonic stress?
– normal, thrust and strike-slip regimes
– no shear stress at the Earth’s surface (shear stress cannot
occur in fluids), one of the principal stresses has to be vertical,
implying that the other two are horizontal.
differentiate total stress and effective stress.
- Total stress (σ) is equal to the sum of effective stress (σ’) and pore water
pressure (u) or, - alternatively, effective stress is equal to total stress minus pore water
pressure.
refer slide no. 18.
what is mean stress and deviatoric stress?
- Mean stress,
gives an average measure of stress. - Deviatoric stress is the difference
between the mean stress and the total stress - The deviatoric stress tensor
represents the anisotropic
component
define rheology.
refers to the flow of matter, primarily in
the liquid state, but also as ‘soft solids’ or solids under
conditions in which they respond with plastic flow rather
than deforming elastically in response to an applied force - temperature-dependant
differentiate elasticity, plasticity, and faulting.
Elasticity
-Hooke’s Law, elongation = strain
-Strain is not permanent
-Faulting = sliding/shearing, need to overcome
the frictional resistance
-earthquake -> release the shearing, rock bounce
back
Plasticity
-Strain is permanent
-Rock does not rupture by faulting, but the
surrounding rocks may permanently distort
Faulting occurred in:
-Weak material (e.g. shale) zone: less resistance
- Stronger material zone: more resistance
Relate temperature and rock type with the rheology.
Higher temperature, and the elasticity gradually lose
Rheology is temperature-dependant
Plastically deform -> creep
Deeper part of the earth, tend to plastic deformation - Temperature > 70% of melting point, the rock tends to deform plastically.
explain Mohr circle.
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