brittle structures Flashcards

1
Q

–The
permanent change that occurs in a
solid material due to the growth of
fractures and/ or due to sliding on
fractures.

A

Brittle deformation

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2
Q
  • 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.
A

Brittle fault zone

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3
Q

A single surface on which movement occurs specifically by brittle deformation mechanisms.

A

Brittle fault-

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4
Q

A deformation process that involves distributed fracturing, crushing, and frictional sliding of grains or
of rock fragments.

A

Cataclasis-

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5
Q

Verb: to break or snap apart. Noun: a fracture whose displacement does not involve shear displacement
(i.e., a joint or microjoint).

A

Crack-

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6
Q

Broad sense: a surface or zone across which there has been measurable sliding parallel to the surface.

A

Fault-

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7
Q

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.

A

Fracture zone

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8
Q

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.

A

Fracture-

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9
Q

A microcrack that has cemented back together. Under a microscope, it is defined by

A

Healed microcrack-

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10
Q

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.

A

Joint-

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11
Q

A very small fracture of any type. _____________ range in size from the dimensions of a
single grain to the dimensions of a thin section.

A

Microfracture-

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12
Q

_________________________ range in size from the dimensions of a single grain to the
dimensions of a hand-specimen.

A

Microjoint-

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13
Q
  • 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).
A

Shear fracture

-* Shear joint-

  • Shear rupture
  • Shear zone
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14
Q

– 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

A

Fracture trace

  • Fracture front
  • Fracture tip
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