8. Deformation and Strain

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23 Terms

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Deformation

A transformation from an initial to a final geometry by means of rigid body translation, rigid body rotation, strain (distortion) and/or volume change

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Strain

Any change in shape with or without change in volume, is referred to as strain, and implies that particles in a rock have changed positions relative to each other

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Stress

Stress on a surface is the force over the area on which it is applied to cause the deformation

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Coordinate Axes

Arbitrary axes in space that we use to describe the motion and length/shape change

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Translation

The body is moved horizontally and/or vertically from its original location

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Rotation

The body is rotated about its original location against a point

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Simple Shear

Non coaxial deformation where the material lines rotate after deformation

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Pure Shear

Coaxial deformation where material lines before and after deformation remain parallel

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Strain Ellipse

The deformed shape of a circle, can measure deformation lines in accordance to original circle of unit radius

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Homogeneous Deformation

Strain (change in shape and/or size) for each small part of the body are geometrically similar to that of the whole body

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Heterogeneous Deformation

Strain where a rock body changes shape, size, or orientation unevenly, so different parts deform differently

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e

Extension, e = (l – l0) / l0

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s

Stretch, s = l / l0, s = 1+ e

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l0

Original length of line

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l

Finite (end) length of line

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Principal Axes

Major/minor axes of strain ellipse

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3D General/Triaxial Strain

Strain where X > Y > Z (plane strain ellipsoid)

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2D Planar Strain

Strain where X > 1 > Z

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1D Simple Shortening/Volume Change

Strain where 1 > Z

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3D Axially Symmetric Shortening

Z-axis oblate strain where X = Y > Z

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3D Axially Symmetric Extension

X-axis prolate strain where X > Y = Z

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Flinn Diagram

A graphical representation of the full range of three-dimensional strain states in deformed rocks, with or without a change in their volume

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Deformation

A transformation from an initial to a final geometry by means of rigid body translation, rigid body rotation, strain (distortion) and/or volume change

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