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GLG310 Structural Geology

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Announcements. Reminder: Application exercise on Tuesday, Sept. 17 in class How do videos look and work? Homework questions?. Strain and deformation. Stretch (strain) ellipse Rotation of lines in deformation Pure and simple shear Progressive deformation Deformation by change of volume. - PowerPoint PPT Presentation

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Page 1: Announcements

GLG310 Structural Geology

Page 2: Announcements

Announcements

• Reminder: Application exercise on Tuesday, Sept. 17 in class

• How do videos look and work?

• Homework questions?

April 21, 2023 GLG310 Structural Geology

Page 3: Announcements

Strain and deformation

• Stretch (strain) ellipse

• Rotation of lines in deformation

• Pure and simple shear

• Progressive deformation

• Deformation by change of volume

April 21, 2023 GLG310 Structural Geology

Page 4: Announcements

April 21, 2023 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

Page 5: Announcements

April 21, 2023 GLG310 Structural Geology

Principal stretches

SphereEllipsoid

In 3D, S1 is max, S3 is min, and S2 is intermediate

Cube Prism

Page 6: Announcements

April 21, 2023 GLG310 Structural Geology

Deformed trilobites do exist!

Draw the stretch ellipse for each

Page 7: Announcements

April 21, 2023 GLG310 Structural Geology

Page 8: Announcements

GLG310 Structural Geology

Page 9: Announcements

Angular shear

Page 10: Announcements

April 21, 2023 GLG310 Structural Geology

Page 11: Announcements

April 21, 2023 GLG310 Structural Geology

Page 12: Announcements

“Coaxial deformation”: Lines parallel to principle axes do not rotate

“Pure Shear”

Page 13: Announcements

April 21, 2023

“Non-Coaxial deformation”: Principle axes are constant but lines rotate with progressive deformation

“Simple Shear”

Page 14: Announcements

Progressive deformation

Page 15: Announcements

Cloos’ strain study

Page 16: Announcements

GLG310 Structural Geology

Measured stretch ratios in rocks from around the world

“Flattening” More common

“Con

stri

ctio

n”

-Suppe, 1985

Page 17: Announcements

Deformation by loss of material-dissolution-”styolites”

http://www.earth.lsa.umich.edu/~vdpluijm/animations/stylolite.mov

http://www.geol.umd.edu/~jmerck/geol100/images/15/stylolite.jpg

Page 18: Announcements

April 21, 2023 GLG310 Structural Geology

Stylolite: Wave-like or tooth-like, serrated, interlocking surfaces most commonly seen in carbonate and quartz-rich rocks that contain concentrated insoluble residue such as clay minerals and iron oxides. Stylolites are thought to form by pressure solution, a dissolution process that reduces pore space under pressure during diagenesis.

Schlumberger Oilfield Glossary http://www.glossary.oilfield.slb.com/Display.cfm?Term=stylolite

Page 20: Announcements

April 21, 2023 GLG310 Structural Geology

Page 21: Announcements

GLG310 Structural Geology

Pro

gres

sive

str

ain

His

tory

of

regi

onal

def

orm

atio

n in

so

uth

ern

Ari

zon

a

Page 22: Announcements

Stretching and Shortening working together in partnership

-Pollard and Fletcher, Fundamentals of Structural Geology, 2005