Week 7 Flashcards

1
Q

F=

A

ma

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2
Q

Newton’s 3rd law

A

equal and opposite reactions

Interactions BETWEEN bodies

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3
Q

Is strain internal or external

A

Internal

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4
Q

What is the internal distribution of forces within an object?

A

Stress

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5
Q

Body stress =

A

Force/unit vol

= act upon and proportional to mass

e.g. gravity

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6
Q

Surface stress =

A

“stresses on a surface”

Force/unit area

= act across real/imagined surfaces and can vary within

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7
Q

What surfaces do geological bodies interact along?

A

Plate boundaries

Faults

Bedding planes

Joints

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8
Q

σ =

A

F/A

Units = N/m2 = Pa

F = vector therefore σ = vector
i.e. has magnitude/orientation

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9
Q

1MPa =

A

10 bars

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10
Q

100 MPa =

A

1kbar

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11
Q

What happens to σ when you increase A?

A

A = “size of area of action”

Decreases σ

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12
Q

Resolving σ

A

σn = normal stress = σcos^2θ
- perpendicular to surface

σs = shear stress = σsin2θ/2
- // to surface

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13
Q

θ =

A

angle between stress vector and surface of action

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14
Q

How do σn, σs, Fn and Fs vary as θ varies from 0-90?

A

σn decreases, Fn decreases

σs peaks at 45’, Fs increases

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15
Q

Planes at 45’

A

EXPERIENCE THE MAX SHEAR STRESS

  • will reach critical condition for failure quicker
  • if shear stress is the only thing affecting the fault will be at 45’
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16
Q

Stress ellipsoid

A

σ1 >= σ2 >=σ3

All normal stresses
Principal stresses
Principal planes of stress
Perpendicular
σs = 0
17
Q

Stress tensor components

A

x,y,z reference system

σ2,1

Stress in the ‘2’ plane (perpendicular to that axis) acting in the ‘1’ direction

18
Q

Hydrostatic stress

A

When σ1 = σ2 = σ3

SPHERE

Isotropic

σn = σ1 = σ2 = σ3
σs = 0

Only volume changes

19
Q

Mean stress

A

Isotropic

σm = (σ1+σ2+σ3)/3

20
Q

Measuring the departure of the stress state from a hydrostatic state

A

DEVIATORIC STRESS
- shape changes (distortions)

σ1-σm

σ2-σm

σ3-σm

21
Q

Differential stress

A

σ1-σ3

Used for fracturing behaviour

22
Q

Stresses on planes; orientation of σ2

A

Assumed // to plane

23
Q

Stresses on planes; σn =

A

(σ1+σ3)/2 + cosθ(σ1-σ3)/2

24
Q

Stresses on planes; σs =

A

sin2θ(σ1-σ3)/2

25
Stresses on planes; what do the equations for σn and σs lead to
A pair of planes at σs max at 45' to σ1 and σ3, intersecting // to σ2
26
Types of fracture
1. MODE II 2. MODE II/III Require a tensile σ3 (-ve)
27
Mode II/III fractures
SHEAR fractures, form at an angle to σ1 = faults
28
Mode I fractures
TENSILE fractures // to σ1σ2 plane, open // to σ3 = joints/veins/dykes
29
Tensile σ3
-ve Rare within Earth (σn is normally compressive, +ve) Effective tension arises where over pressurised fluid is injected along fractures to a pressure > σ3
30
What does a mean tectonic transport direction of 100' to 280' mean?
Top-to-the-west overthursting
31
POINT MAXIMUM When points represent: a) lines b) poles to planes
a) linear preferred orientation | b) planar preferred orientation
32
GREAT CIRCLE GIRDLE DISTRIBUTION When points represent: a) lines b) poles to planes
a) planar preferred orientation (all lines lie in common plane) b) linear preferred orientation (all planes contain a common line; beta axis (=regional fold axis))
33
GIRDLES MAY SHOW POINT MAXIMA When points represent: a) lines b) poles to planes
a) some lines also have linear preferred orientation | b) some planes also have planar preferred orientation (=fold limbs)
34
Why do all natural datasets display spread?
Inaccurate measuremnets Natural irregularity of structures Dispersion of data due to later deformations Curvilinear/curviplanar geometries
35
Sheath fold
Initially slightly curved fold hinge line becomes accentuated by intense ductile shearing and strain Fold hinges progressively rotated round into parallelism with mineral lineation (=X axis of finite strain) Eye structures are common
36
Where are the maximum and minimum normal stresses found?
On surfaces at 0 and 90 degrees to the imposed stress/force
37
Where are the maximum and minimum values of shear stress found?
Max = on planes at 45' to the imposed stress/force Min = at 0 and 90'