Geological Musings
Wednesday, July 17, 2013
Anderson's Theory of Faulting
Assuming that there is no shear stress at the Earth's surface (shear stress cannot occur in fluids), one of the principal stress components must be vertical and thus the other two must be horizontal.
σ
v
=
σ
1
normal fault
σ
v
=
σ
2
reverse fault
σ
v
=
σ
3
strike-slip fault
Anderson's Theory of Faulting
Normal, Reverse, and Strike-Slip Faults
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