Structures (Structural) Flashcards

1
Q

Intracrystalline kink structures that resulted from strain through mechanical twinning, or twin gliding.

A

Deformation Twins

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2
Q

Mechanical bending or kinking of the crystal lattice that resulted from stress. Twin Gliding-Involves simple shear along the twin plane once critical stress is reached.

A

Twinning

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3
Q

A form of crystal defect that may either be vacancies, substitution or interstitial impurities within a crystal lattice.

A

Point Defect

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4
Q

A gap or hole between atomic bonds in crystal lattices.

A

Vacancy

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5
Q

Occurs when a different atom or molecule substitutes the original atom or molecule in its location.

A

Substitution

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6
Q

Impurities that are locked within atoms or molecules of a crystal lattice.

A

Interstitial Impurity

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7
Q

A mobile line defect or dislocation that contributes to intracrystalline deformation by slipping.

A

Line Defects

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8
Q

a diffusion of vacancies through crystals that is temperature- and stress-controlled.

A

Nabarro-Herring Creep or Volume diffusion

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9
Q

A mechanism that involves migration of vacancies in crystallographic lattices.

A
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10
Q

diffusion of vacancies along grain boundaries that is temperature- and stress-controlled.

A

Coble Creep or Grain boundary diffusion

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11
Q

a diffusion that is chemically- and stress-controlled and occurs along a thin film of fluid and pore fluid along grain boundaries.

A

Wet Diffusion

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12
Q

A form of dislocation where an extra half-plane is placed between crystal lattices.

A
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13
Q

A form of dislocation where the dislocation line is parallel to the slip direction, and half-plane of the crystal lattices slides across each other.

A

Screw Dislocation

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14
Q

Any planar or subplanar discontinuity that is very narrow in one dimension compared to the other two and forms as a result of either an external or internal stress.

A

FRACTURE

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15
Q

Extensional fractures filled with air or fluid.

A

Fissure

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16
Q

Fractures that are filled with gas, fluids,
magma or minerals.

A

Extension Fractures

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17
Q

anticracks, are fractures with contractional displacements across the fractures that are filled with residue from the rock.

A

Contractional Fractures

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18
Q

A slip surface fracture along which there is a
large offset movement that is parallel to the fracture.

A

FAULT

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19
Q

The relatively high footwall block between faults where the two adjacent faults dip away from one another.

A

Horst

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20
Q

A fault-bounded block that drops down between two adjacent faults dip toward one another.

A

Graben

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20
Q

A depression created as a consequence of the rotation accompanying displacement on a normal fault and the original top surface of the hanging wall block tilts toward the fault.

A

Half-Graben

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21
Q

The bearing of the imaginary line formed by the intersection of the fault plane with a horizontal plane, found with an equal elevation.

A

Strike

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22
Q

the bearing of the imaginary horizontal line perpendicular to the strike; Angle the vertical angle between an inclined plane and the dip direction, perpendicular to the strike.

A

Dip Direction

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23
Q

The slip surface of a fault.

A

Fault Plane

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24
The rock block resting on top of the fault plane.
Hanging Wall
25
The rock block positioned beneath the fault plane.
Foot Wall
26
The horizontal component of the dip separation measured perpendicular to the strike of the fault.
Heave
27
The vertical component in the vertical plane containing the dip.
Throw
28
The combination of the vertical and horizontal component.
Oblique Slip
29
The total amount of displacement measured parallel to the direction of the motion.
Net Slip
30
the angle formed from an inclined plane between a horizontal line and a line in question.
Rake (B) or Pitch
31
The vertical angle between an inclined plane and a horizontal line that is not perpendicular to the strike of the plane.
Apparent dip
32
For any inclined plane (except a vertical one), the true dip is always greater than any apparent dip.
33
An apparent dip may be defined by its _________ or by its _______ within a plane.
trend and plunge ; pitch
34
The orientation in space of a line or plane.
Attitude
35
By convention, the attitude of a plane is expressed as its strike and dip; the attitude of a line is expressed as trend and plunge.
36
Method of expressing the strikes of planes and trends of line based on a 360° clockwise circle. Azimuthal bearing always starts from the due north.
Azimuth method
37
The horizontal angle between a line and a specified coordinate direction, usually true north or south; the compass direction or azimuth.
Bearing
38
The plunge of the true dip.
Delta
39
The vertical angle between a line and the horizontal.
Plunge
40
Method of expressing strikes of planes and trends of lines based on four 90° quadrants.
Quadrant method
41
The direction (trend) of the apparent dip.
Theta
42
The bearing (compass direction) of a line. Non-horizontal lines trend in the down-plunge direction.
Trend
43
An array of faults in a strike-slip fault zone that merges at depth into a near-vertical fault plane, but near the ground surface diverges so as to have shallower dips.
Positive FLOWER STRUCTURE
44
A flower structure where there is a component of normal faulting.
Negative Flower Structure
45
Occurs where two subparallel thrusts of approximately equal displacement are separated by a deformed interval that is thin relative to its total area extent.
DUPLEX
46
develops where thrust sheet has been antiformally folded, causing part of the sheet to have a higher elevation.
FENSTER Or Window
47
Dismemberment of a thrust sheet by erosion.
KLIPPE
48
A rock that is still in its place of origin; the footwall below a detachment.
AUTOCTHON
49
A rock that has moved from its place of origin; the thrust sheet above a detachment.
ALLOCTHON
50
A structural feature that is formed when planar features are bent or curved.
FOLDS
51
PARTS OF FOLDS
Hinge Hinge Zone Hinge Point Limb Amplitude
52
The gradual, or sharp and abrupt, curvature of the fold. Hinge Line - The line of greatest curvature.
Hinge
53
The area where the fold hinges.
Hinge Zone
54
The point of maximum curvature of the folded layer located within the hinge zone.
Hinge Point
55
The less curved portion of a fold.
Limb
56
Half the height of the fold, measured from the crest to trough.
Amplitude
57
The surface containing the hinge lines from consecutive folded surfaces.
Axial Surface
58
The topographically highest point of a fold, which need not coincide with the fold hinge.
Crest
59
High point of the hinge line in a non-cylindrical fold.
Culmination
60
Fold in which a straight hinge line parallels the fold axis; in other words, the folded surface wraps partway around a cylinder.
Cylindrical Fold
61
Low point of the hinge line in a noncylindrical fold.
Depression
62
Fold generator in cylindrical folds.
Fold Axis
63
The position in a limb where the sense of the curvature changes.
Inflection Point
64
Fold with a curved hinge line.
Non-cylindrical Fold
65
The topographically lowest point of a fold, which need not coincide with the fold hinge.
Trough
66
The distance between two hinges of the same orientation.
Wavelength
67
More or less regularly-shaped rectangular fragments formed by stretching of competent layers or foliations.
BOUDINS
68
The process that leads to the formation of boudins from originally continuous layers.
Boudinage
69
Regularly-spaced areas of thinning in many extended competent layers without the separation into isolated fragments or boudins.
PINCH-AND-SWELL STRUCTURES
70
Circular or elliptical structural or topographic highs in which beds dip away to all directions; when eroded, the oldest rocks are exposed at the center.
DOMES
71
Circular or elliptical structural or topographic lows or downwarps in which beds dip towards the center; when eroded, the youngest rocks are exposed at the center.
Basin
72
the presence of layers with different competencies directly affects the strain pattern in the deforming body and there is contrasting behavior between layers.
Flexural folding Or active folding,
73
A dynamic condition in active folding where the applied force is oriented at an oblique angle to the layering.
Bending
74
The most common situation for folding, is a dynamic condition in active folding where the force is oriented parallel to the mechanical anisotropy.
Buckling