Strain Flashcards

(41 cards)

1
Q

Response of a body to
stress

A

deformaation

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2
Q

Strain is ___________ when any two
portions of the body that were similar in form and orientation remain the same before and after deformation.

A

homogenous

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3
Q

If one or more of these factors are not met, the strain is?

i. Originally straight lines remain straight.
ii. Originally parallel lines remain parallel.
iii. Circle becomes ellipses; spheres become ellipsoids.

A

Heterogenous

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4
Q

Strain variations can be due to the different mechanical behaviors of components of a rock or association of rocks.

One may reduce heterogeneous deformation to homogeneous
domains by decreasing the size of the studied volume.

Presence of relatively rigid components can result in more intense strain concentrated into weaker parts of the rock rather than beiing evenly distributed.

A

Homogenous-heterogenous Strain

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5
Q

T or F
A homogeneous deformation
on one scale may be part of a
heterogeneous deformation
on a different scale.

A

T

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6
Q

Series of movements that affect a body from its initial
undeformed stage to its deformed state.

A

Progressive Deformation

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7
Q

T or F

Progressive deformation cannot be both continuous nor discontinuos.

A

F, they can be.

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8
Q

total strain acquired by a body up to the time of measurement.

A

Strain Rate

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9
Q

intermediate strain steps towards
the final configuration

A

Incremental Strain

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10
Q

each increment can be divided into a series of smaller and smaller increments. When the duration tends to zero, the extremely small amount of strain is termed _____________.

A

Infinitesimal / Instantaneous

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11
Q

measure of strain that compares
the initial and final configurations

A

finite strain

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12
Q

The sequence of strain states through which the object passed during progressive deformation.

A

Strain Path

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13
Q

changes in the lengths of lines

A

linear strain

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14
Q

if elongation is positive, what occured is ________

A

extension

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15
Q

if elongation is negative, what occured is ________

A

shortening

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16
Q

changes in angles of lines

A

Shear Strain

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17
Q

amount a vertical line has
been rotated with respect to
a horizontal line.

A

angular shear

18
Q

changes in volume

A

volumenric strain (dilational strain)

19
Q

If homogeneously strained, a 2D-body will have at least two
___________ __________ that do not rotate relative to each other; their
angle remains the same before and after strain.

A

material lines

20
Q

T or F
A material line
is made up of a series
of points in a body.

21
Q

represents the cumulative,
total deformation;

A

Finite Strain Ellipse

22
Q

represents the strain for an
instant in time.

A

Infinitesimal ellipse

23
Q

Graphical representation to
visualize the amount of linear
and angular strain involved
in the deformation of rock.

A

Strain Ellipse

24
Q

Defined by the longest (X) and shortest (Y) axis = _____________ ___________ ___________

A

principal strain axes

25
represents the direction and magnitude of the maximum stretch (S) and elongation (ε)
stretching axis
26
represents the direction and magnitude of the minimum stretch (S) and elongation (ε).
shortening axis
27
Describes how the shape of an imaginary spherical reference object would be changed as a result of deformation. Defined by three mutually perpendicular finite stretching axes.
Strain Ellipsoid
28
Visualization of the range of possible strain ellipsoid shapes. Separates the prolate from oblate geometries.
Flinn Diagram
29
field of stretching/ (constriction)
prolate
30
field of flflattening
oblate
31
state where one of the strain axes (Y) is of the same length before and after strain. Deformation only occurs along X and Z axes.
Plane Strain
32
If the strain axes have the same orientation as they did before deformation started, then the deformation is ______-___________.
Non-Rotational
33
If the strain axes does not have the same orientation as they did before deformation started, then the deformation is ___________.
rotational
34
If the strain increments are all non-rotational, then the strain axes maintain their same direction as they had in the undeformed state. Strain axes remain parallel to the same material lines throughout straining.
Coaxial Deformation
35
Contraction and elongation are parallel to the strain axes, so there will be no rotation of the axes from their original positions.
Pure shear
36
The directions of the principal strain axes rotate through different material lines at each infinitesimal strain increment. The axes of the finite and infinitesimal strain ellipses are not parallel.
Non-coaxial deformation
37
During deformation, the strain axes rotate. The amount of rotation depends on amount of strain; the greater the strain, the greater the rotation.
Simple shear
38
Strain can be retrieved from rocks through a range of different methods. It can be using 1D, 2D and 3D strain analyses in deformed rocks. Strain analyses gives us an opportunity to explore the state of strain in a rock and to map out strain variations in a sample, an outcrop or a region. The shape and orientation of the strain ellipse or ellipsoid may also contain information about how the deformation occurred.
Strain Analysis
39
Examples (of ________ _________) indicating change in length: i. Boudinaged dikes or layers. ii. Minerals or linear fossils (i.e., belemnites or graptolites that have been elongated).
strain markers
40
Based on the principle that before deformation, the centers of the spherical objects had an isotropic and uniform distribution. When a set of point with statistically uniform distribution is deformed, the average distance between the neighboring points in any direction increases or decreases in the same ratio as the length of a marker in that direction.
Fry Method
41
based on the angular distortion of reference lines originally aligned 90° to each other.
wellman method