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Shear zone: zone of highly strained rocks
A fault zone is a shear zone formed in the brittle regime
Can also have a purely ductile shear zone
Or even a zone with a mixture of brittle and ductile deformation- due to composition (feldspar or qtz) or strain rate (silly putty analogy)
Shear zones form in the deeper crust of all
structural systems: thrust, strike-slip and normal
But how are they brought to the surface (exhumed)?
"Tectonic Exhumation"
Removal of
overburden by normal faulting.
Erosion plays a role, but is not
required!
brittle fault offsets- be careful!!!!
1) faults postdate ductile deformation2) sense of shear not always clear
Mica-fish fabrics. Typical for sheared rocks with muscovite and/or biotite. A special form of S-C fabric. Again wings/tails step up in direction of shear
So far, we have talked about shear fabrics related to noncoaxial deformation (simple shear).
Some "shear" zones are not due to simple shear, but rather coaxial deformation (pure shear)
What do some of these structures look like?