glg310 structural geology - arizona state...
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GLG310 Structural Geology
4 September 2013 http://vyanks.blogspot.com/2010/08/traffic-jams.html
Vectors
Coordinate
Length
Direction
Components
Addition
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4 September 2013 http://vyanks.blogspot.com/2010/08/traffic-jams.html
Vectors
Coordinate
Length
Direction
Components
Addition
4 September 2013 http://vyanks.blogspot.com/2010/08/traffic-jams.html
Vectors
Coordinate
Length
Direction
Components
Addition
3
4 September 2013 http://vyanks.blogspot.com/2010/08/traffic-jams.html
Vectors
Coordinate
Length
Direction
Components
Addition
4 September 2013 GLG310 Structural Geology
Displacement vector
Position 1: x1,y1,z1
Position 2: x2,y2,z2
Dx =
Dy =
Dz =
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4 September 2013 GLG310 Structural Geology
Displacement field
(continuous and uniform)
4 September 2013 GLG310 Structural Geology
Displacement field
(continuous and nonuniform)
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4 September 2013 GLG310 Structural Geology
Displacement field
(discontinuous and nonuniform)
Discontinuity
GLG310 Structural Geology
Deformation and
displacement gradients
profile
Displacement
vectors caused by
dike inflation at
Kilauea
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4 September 2013
Consider a profile from point 1 to point 2:
x locations
u is velocity. x and u are positively increasing to the right
4 September 2013 GLG310 Structural Geology
Deformation rates
If we take the Kilauea example as a representative geologic
deformation rate (and it is), how long would it take to build a
structure like that shown below?
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4 September 2013 GLG310 Structural Geology
7.5x105 yr
750,000 yrs!
GLG310 Structural Geology
Determine the magnitude of shortening (e) of this bed assuming
that it was originally planar
If a reasonable shortening rate is –1 x 10-7/yr, how long would it
take to make these folds?
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4 September 2013 GLG310 Structural Geology
Moving from 1 to 2 to 3
dimensional deformation • E and s as we have
defined them in the last two lectures are 1 dimensional (measured along lf).
• In a deformed material; however, we can define the minimum and maximum stretches and they will be perpendicular
Smin=lfmin/l0
Smax=lfmax/l0
l0
l0
lfmax
lfmin
4 September 2013 GLG310 Structural Geology
Principal stretches
Sphere Ellipsoid
In 3D, S1 is max,
S3 is min, and S2 is
intermediate
Cube Prism
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GLG310 Structural Geology
Measured stretch ratios in rocks from
around the world
“Flattening”
More common
“C
on
stri
ctio
n”
-Suppe, 1985
4 September 2013 GLG310 Structural Geology
Deformed
trilobites
do exist!
Draw the
stretch
ellipse for
each