Deformation Mechanisms and Microstructures Flashcards

1
Q

microscale deformation mechanisms that occurs within individual mineral grains

A

Intracrystalline deformation

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2
Q

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

A

Intercystalline deformation

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3
Q

strain expression of mechanical bending or kinking of the crystal lattice particularly at very low temepratures Pagioclase and calcite

A

Deformation twins

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4
Q

The process of forming deformation twins

A

mechanical twinning

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5
Q

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.

A

Calcite

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6
Q

True or False: The more defects in a crystal lattice wether deformed or not, the higher the stored energy.

A

True

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7
Q

Movement of vacancies

A

Diffusion

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8
Q

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

A

Point defect

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9
Q

a mobile line defect that contributes to intracrystalline deformation by a mechanism called slip ( movement of dislcation font within a plane)

A

Line defects/dislocation

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10
Q

is a mechanism involving migration of vacancies in crystallograpic in crystallograpic lattices

A

Diffusion or creep

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11
Q

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.

A

Nabarro - Herring Creep

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12
Q

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

A

fabric or strain

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13
Q

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

A

True

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14
Q

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

A

Grain Boundary-Coble creep

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15
Q

bears similarity to Coble Creep and geometrically and mathematically it can be treated in the same way.

A

Pressure solution or wet diffusion

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16
Q

whats the difference between pressure solution and Coble creep?

A

diffusion occurs along a thin film of fluid along grain boundaries (solution seam)

17
Q

Wet diffusion is a microdeformation mechanism that results to volume reduction. This mechanism is what is known as,

A

chemical compaction

18
Q

a mobile line defect that contributes to intracystalline deformation by a mechanism called slip —– which, implies, movement of a dislocation front within a plane

A

dislocation

19
Q

Give the specific control for volume diffusion where vacancies move through crystals

A

temperature and stress

20
Q

controls for grain boundary; where vacancies move along grain boundaries

A

temperature and stress

21
Q

what are the controls for Pressure solution? where ions move in fluid films and pore fluid?

A

chemically and stress controlled

22
Q

is a type of dislocation that edge is an extra plane half plane of the crystal lattice

A

edge dislocation

23
Q

a dislocation line that is oriented parallele to the slip direction

A

screw dislocation

24
Q

the formation, motion and destruction of dislocations in a crystals

A

dislocation creep

25
Q

The process by which edge dislocations move

A

dislocation glide

26
Q

True or false: Dislocation creeps allows the deformation to take place at much lower differential stress that required for brittle fracturing

A

True

27
Q

True or false: Dislocation movements weaken or damage a mineral

A

false

28
Q

These are atomic-scale deformation structures such as dislocations can only be studied by means of electron microscopy at 10 000-100000x mg. They are reffered as microstructures and carry information about temperature, state of stress and rheological properties at the time of deformation

A

Microstructures