structural geology (week 2) Flashcards

(44 cards)

1
Q

what is deformation

A
  • causes rocks to change shape, size, location or orientation
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2
Q

what analysis can be performed on deformed rocks

A
  • descriptive
  • kinematic, where changes in position or shape of the rock
  • dynamic, where forces/stress acting on rock *rheology
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3
Q

how are things kinematically analysed

A
  • motion of objects
  • interpret deformational movements
  • translation, distortion, rotation, dilation and dilation
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4
Q

what is stress

A
  • is the force applied to a given area and is defined per unit area
  • stress= force/area
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5
Q

what is differential stress

A
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6
Q

what is stress ellipsoid

A
  • maximum extension occurs when stress=3
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7
Q

what is strain ellipsoid

A
  • when maximum compression occurs towards stress=1
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8
Q

what are the two types of strain and how is it formed

A
  • product of stress
  • brittle- cracking/fracturing
    -ductile- bending and flowing
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9
Q

co axial vs non co axial

A

-CO AXIAL
-horizontal stretching/ shortening

NON CO AXIAL
- shear strain

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10
Q

is a pure shear co axial or non-coaxial

A

co-axial

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11
Q

is a simple shear co axial or non-coaxial

A
  • non co axial
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12
Q

under what conditions does brittle and ductile deformation occur

A

low temperature= brittle
high temperature= ductile

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13
Q

deformation style is dependant of rheology, what factors come into play

A
  • temperature
  • minerology
  • grain size
  • rock fabric
  • fluids
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14
Q

how can strength be quantified in rocks

A
  • a compression rig can be used to yield the strength of rocks and soils
  • 3 principal axis of strength
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15
Q

how can the failure envelope be calculated

A
  • based on representative rig compression results
  • ## represents the force needed to cause a specific material to fail (fracture)
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16
Q

a very important example of modelled stress in rocks

A
  • the shakespeare cliff
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17
Q

what is a fault

A

-ma structural break in a rock across which there is notable dispacement

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18
Q

what is a joint

A
  • fractures which have no notable displacement
    important in engineering geology
19
Q

two examples of faults

A
  • highland boundary fault
  • moine thrust
20
Q

fault rock to describe the moine thrust

21
Q

what are the 3 main types of fault movements

A
  • dip slip
  • oblique- slip fault
  • strike- slip
22
Q

what are the types of dip slip faults

A
  • normal fault
  • reverse fault
23
Q

what is a normal fault

A
  • hanging wall block moves down relative to the footwall
  • extension of the earths crust thins the crust
24
Q

what are reverse dip-slip and thrust faults

A
  • hanging wall block moves up relative to the footwall
  • results in compression of the earths crust= thickens the crust
  • ## reverse faults are steeper than thrust faults
25
how do faults work as mineralisation zones
- precipitation of ore minerals can occur within the fault and surrounding fractures
26
how do faults operate as conduits
- formation of hydrothermal ore deposits on the seafloor from fluid transport along faults
27
what are horst and graben structures
- normal fault bounded valleys= grabens -normal fault bounded ridges=horsts for example, the basin and range province, in western USA
28
how are mountain belts formed
- compression- thrust faults- mountain belts
29
what is the process in which mountain belts build
orogenesis
30
how do sinistral strike slip faults
- sinistral - (left lateral) strata on the opposite side of the fault plane is displaced on the left - dextral- (right lateral) - strata on the opposite side of the fault plane is displaced to the right
31
how do faults operate as conduits
provide natural resources as hydrothermal ore deposits on the seafloor due to fluid transport along faults
32
how do ores operate as mineralisation zones
- precipitation of ore minerals can occur within the fault and the surrounding fractures
33
what deposit provides gold to the scotgold resource Limited
cononish
34
what is strike
- orientation of a horizontal line on a planar structure
35
what is dip
-angle of inclination on a planar structure
36
what is dip direction
- the compass direction in which the planar structure is dipping
37
how do folds form
- caused by compression stress parallel to the bedding planes in a rock body - ductile deformation process-very slow process (avg= 100,000 years to several mill)
38
ANATOMY OF A FOLD
- hinge- zone of max curvature - hinge line- line of maximum curvature
39
what can be used to quantify tightness
- interlimb angle - shows how much distrotion a rock has experienced
40
what is the axial trace
- where the axial plane intersects the earths surface
41
whats an antiform
- fold closes upwards (angry)
42
whats a synform
- fold closes downwards (smiley!)
43
old rocks in the fold core
synformal anticline
44
young rocks in the core of the fold
antiformal syncline