brittle structures Flashcards
–The
permanent change that occurs in a
solid material due to the growth of
fractures and/ or due to sliding on
fractures.
Brittle deformation
- A band of finite width in which slip is distributed among many smaller discrete brittle faults,
and/or in which the fault surface is bordered by pervasively fractured rock.
Brittle fault zone
A single surface on which movement occurs specifically by brittle deformation mechanisms.
Brittle fault-
A deformation process that involves distributed fracturing, crushing, and frictional sliding of grains or
of rock fragments.
Cataclasis-
Verb: to break or snap apart. Noun: a fracture whose displacement does not involve shear displacement
(i.e., a joint or microjoint).
Crack-
Broad sense: a surface or zone across which there has been measurable sliding parallel to the surface.
Fault-
A band in which there are many parallel or subparallel fractures. If the fractures are wavy, they
may anastomose with one another. Note: The term has a somewhat different meaning in the context of ocean-
floor tectonics.
Fracture zone
A general term for a surface in a material across which there has been loss of continuity and,
therefore, strength. Fractures range in size from grain-scale to continent-scale.
Fracture-
A microcrack that has cemented back together. Under a microscope, it is defined by
Healed microcrack-
A natural fracture which forms by tensile loading, i.e., the walls of the fracture move apart very
slightly as the joint develops. Note: A minority of geologists argue that joints can form due to shear loading.
Joint-
A very small fracture of any type. _____________ range in size from the dimensions of a
single grain to the dimensions of a thin section.
Microfracture-
_________________________ range in size from the dimensions of a single grain to the
dimensions of a hand-specimen.
Microjoint-
- A macroscopic fracture that grows in association with a component of shear parallel to
the fracture. Shear fracturing involves coalescence of microcracks.
A surface that originated as a joint but later became a surface of sliding.
- A shear fracture.
- A region of finite width in which ductile shear strain is significantly greater than in the
surrounding rock. Movement in shear zones is a consequence of ductile deformation mechanisms
(cataclasis, crystal plasticity, diffusion).
Shear fracture
-* Shear joint-
- Shear rupture
- Shear zone
– the line representing the
intersection of the fracture with the surface of a
rock body.
– the line that separates the
region of the rock which has fractured from the
region that has not fractured.
– the point at which the fracture
trace terminates on the surface of the rock
Fracture trace
- Fracture front
- Fracture tip