2. Shear zones and shear sense indicators Please read (D&R, pp. 493-551)

3. 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)

5. But how are they brought to the surface (exhumed)?
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)?

6. Thrusting must be accompanied by erosion to cause exhumation

7. Removal of overburden by normal faulting.
"Tectonic Exhumation"
Removal of overburden by normal faulting.
Erosion plays a role, but is not required!

8. The architecture of many extensional shear zones
brittle detachment fault

9. A ledge of fault breccia below the detachment

10. thick zone of mylonitic rocks below the detachment

11. Ahh, sweet mylonites! What is sense of shear?

12. Even deeper- a less deformed "injection complex"

13. Undeformed granite in core
Mylonite

14. Shear sense indicators in shear zones

15. brittle fault offsets- be careful!!!!
1) faults postdate ductile deformation
2) sense of shear not always clear

16. ductile offsets within shear zone- better!

17. another example of a small ductile shear zone

18. Folds, transposition, and ambiguous sense of shear

19. sheath folds (tongues that point in direction of shear)

20. Cross section of a sheath fold

21. Mylonites are EXCELLENT! What is sense of shear?
Porphyroclasts

22. Sigma structure- wings step up in direction of shear

23. Delta structure: porphyroclast rotates faster than wings

24. Delta structure: porphyroclast rotates faster than wings

25. A delta + sigma structure- what is sense of shear?

26. 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

27. Fish often occur in schools

28. Pressure shadows: Pressure solution in zones of high stress; recrystallization in zones of low stress- inclined in direction of shear
top to left sense of shear

29. Summary of shear fabrics

30. 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?

31. symmetric boudins due to flattening/stretching

32. Symmetric pressure shadows due to flattening (pure shear) strain

33. Next Lecture: Deformation mechanisms and microstructures Please skim Chapter 4 of Davis and Reynolds to get familiar with terminology and figures