2. What is a shear zone?
Shear zones can be quite similar to faults and
thus confusing, but a simple definition for
shear zones:
A tabular zone in which strain is noticeably
higher than in the surrounding rock
3. Shear Zones vs. Faulting
But wait, that sounded like a definition for a fault as well?
It is, however, a fault is a special case of shear zone where
brittle deformation occurs:
A ‘traditional’ shear zone is one where ductile deformation
occurs (plastic). Some facts:
Shear zones have a thickness relative to displacement
Fault zone cores are thinner than a standard shear zone
Variation of strain in a shear zone is more gradual than in
faults
Shear zones can occur under pure shear and simple shear
conditions
Microscale deformation can occur either plastically or ductily.
5. Geometry and
Thickness
Graph above shows how
shear zones possess a
relatively thicker
deformation zone over
fault cores.
However, thickness in
shear zones is comparable
to the entire damage zone
(fractured region
surrounding the fault core)
6. Shear Zone Mechanisms
Simple shear vs. pure shear
Remember, pure shear is not
rotational.
Simple shear is rotational
7. Shear Zone Brittle vs.
Ductile
Ideal shear zones = perfectly ductile and involve
simple shear with or without additional
compaction/dilation
No discontinuities/slip surfaces should exist under this
criteria
Passive markers (i.e. something that indicates
displacement) can be traced continuously through a
perfectly ductile shear zone
8. Shear Zone Brittle vs.
Ductile
A perfectly ductile shear zone
contains no internal
discontinuities
Many plastically deformed
shear zones show sharp
internal discontinuities in the
form of slip surfaces,
extension fractures, and veins
= these are called semi-
ductile
9. Examples:
Note flattening and rotation of grains
as enter the main shear zone
This indicates that the
feldspar crystals are
becoming progressively
more strained into the shear
zone.
(and satisfies the shear zone
definition)
13. Direction of Shear
Asymmetry of mylonites
can be used to evaluate
the sense of shear and
sometimes also the
degree of coaxiality of a
mylonite zone
Development of S-C
structures:
1. Newly formed foliation S
is cut by shear surface C.
2. Continued deformation
rotates S so that it is
close to parallelism with
C, known as CS-foliation.
3. New and oblique shear
bands C’ form and back-
15. Sense of Shear -
Porphyroclasts
σ type – do not cross reference line
δ type – do cross reference line
φ type – symmetric about reference line
16. Sense of Shear - Porphyroclasts
σ types and δ types can indicate the sense or direction
of shear in a similar way to the mica fish (tails point in
direction of shear), this allows us to identify if the
shear zone is left-lateral (sinistral) or right-lateral
(dextral).
17. Sense of Shear - Porphyroclasts
φ types occur during coaxial deformation (pure
shear; no rotation)
18. Sense of Shear - Porphyroclasts
Synthetic fracture of porphyroclasts can also
define sense of shear (like a Riedel-Shear in strike-
slip faults these will be at low angle in relation to
the shear zone)
Antithetic fractures also occur [like antithetic R-
shears (R’ -shears), these will be at high angle to
the shear zone]
Tiling – an imbrication of clasts, note that stepping
occurs consistently in same direction.
Synthetic fracture
of porphyroclast
Tiling
Antithetic
fracture
23. Quarter Structures
σ1
σ1
σ3
σ
3
Local thickening and
thinning can occur around
a clast in a shear zone in
accordance with the
extensional and
contractional quadrants,
respectively
This is due to the fact that
matrix shear zone material
must accelerate past the
clast on the thinning side
and as the material moves
to the extensional side, it
accretes as it decelerates
24. Tension Gashes
Extensional veins (small
fractures) can occur in the shear
zones and are often filled in due
to mineralisation
These align parallel to σ1,
because the fractures open
parallel to σ3 (the instantaneous
stretching axis)
Thus they can be used to
determine shear sense
Over time, the shear sense will
cause tension gashes to fold as
in (b)
Form en echelon patterns