brittle deformation

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Brittle Deformation. Remember that q is the angle between s 3 and a plane. Definitions. Differential Stress: Difference between largest and smallest stresses Deviatoric Stress: Difference between total stress and mean stress. s 1. Magnitude of Normal and Shear Stresses. Normal. - PowerPoint PPT Presentation

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Page 1: Brittle Deformation
Page 2: Brittle Deformation

Brittle Deformation

Remember that q is the anglebetween s 3 and a plane

Page 3: Brittle Deformation

Definitions

Differential Stress: Difference between largest and smallest stresses

Deviatoric Stress: Difference between total stress and meanstress.

Page 4: Brittle Deformation

Magnitude of Normal and

Shear Stresses

s1

s3

Normal

Shear

Page 5: Brittle Deformation

What does this mean for fractures?

Fractures will form when sn is low but ss is high.

q is usually 60° when fractures form

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Coulomb Fracture Criterion predicts failure in rock:

ss = sn tanf

f is the angle of internal friction

tan f is the coefficient of internal friction

Rocks: Avg. is 0.6

C is the point at which sn = 0T is the point at which ss = 0

q = 90° -2f

Page 8: Brittle Deformation

Shaded area is stable(No brittle failure)

No failure

Failure

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ExerciseSketch two cross sections:In one, s1 is horizontal, s3 vertical What is the dip of the fault predictedby this model?

In the other s3 is horizontal, s1 vertical . What is the dip of the fault?

Remember that q is the angle between s 3 and the plane. See also fig. 6.16.

Page 11: Brittle Deformation

Frictional SlidingOnce a fracture exists deformation continues by frictional sliding or cataclastic flow

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CCW Rotation

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Formation of Shear Fractures

s3

s1

2 faults form

1 fault stays active

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Crack is Parallel to s1 These two are not faults.

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Shallow crust

Deep crust

Page 18: Brittle Deformation

Non-frictional sliding on Fault surface: Calcite fibers from fluids in fault zone