Exam 1 Chapters 1-3 Flashcards

1
Q

How do we examine deformation?

A

Through geometric, kinematic, and dynamic analysis

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2
Q

What is geometric analysis?

A

Examine deformation through shape, orientation, and size

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3
Q

What is kinematic deformation?

A

Examines deformation through the description of motion and displacement

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4
Q

What is dynamic analysis?

A

Examines deformation through the study of forces causing deformation (separates observations from interpretations)

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5
Q

What does a tectonic plate consist of

A

the crust and the upper mantle (lithosphere)

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6
Q

Crust thickness

A

7-70km

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7
Q

Mantle thickness

A

~2900km

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8
Q

Core thickness

A

2900-6370km

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9
Q

3 compositonal layers of the earth

A

crust, mantle, core

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10
Q

5 rheological layers of the earth

A

lithosphere, asthenosphere, lower mantle, outer core, inner core

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11
Q

What are transformations?

A

describe how original locations, orientations, shapes and/or sizes of volumes of rock or material points within volumes of rock become changed

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12
Q

what are the four kinds of transformations?

A

translation, rotation, dilation, and distortion

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13
Q

Rotation

A

a rotation of material points about some common axis

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14
Q

translation

A

all points in a body move the same distance along parallel paths

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15
Q

dilation

A

a change in size without a change in shape

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16
Q

distortion

A

a change in shape of a body of rock

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17
Q

rigid body deformation

A

each point within the body of rock maintains the same location related to the other points
- translation and rotation

18
Q

non-rigid body deformation

A

the spacing of points within the body of rock change with respect to one another
- dilation and distortion

19
Q

strain

A

results from non-rigid body deformation through change in size or shape
- results from change in spatial arrangement

20
Q

Primary structures

A

develop during the formation of a rock body

21
Q

examples of primary structures

A

cross bedding, ripple marks, graded bedding, ropy texture in basalt

22
Q

secondary structures

A

develop in rocks after their formation

23
Q

mohorovic discontinuity

A

the boundary between the earths crust and the mantle

24
Q

angular shear

A

measure of the change in angles between lines

25
Q

clockwise rotation

A

negative

26
Q

counterclockwise rotation

A

positive

27
Q

strain ellipse

A

distortion acuminated by a geologic body as a result of deformation

28
Q

what are S1 and S3

A

the principal axes of the finite strain ellipse

29
Q

S1

A

the long axis of the finite strain ellipse and the direction of maximum finite stretch

30
Q

S3

A

the short axis of the finite strain ellipse and the direction of minimum finite stretch

31
Q

plane strain

A
  • the strain is two dimensional
  • neither stretching or shortening in direction perpendicular to the plane that contains the directions of maximum and minimum finite stretch
32
Q

end case of coaxial deformation

A

pure shear

33
Q

coaxial deformation

A

lines that at the very first instant of deformation were aligned parallel to the direction of the long and short axes of strain (s1 and s3) will remain mutually perpendicular and parallel to the the long and short axes of the strain ellipse throughout the deformation

34
Q

pure shear

A

extension of the material will be balanced by the shortening

35
Q

non coaxial deformation

A

all particles move parallel to the direction of shearing but the directions of greatest stretch (s1) and least stretch (s3) continuously change, oblique to the direction of shearing

36
Q

what is used to portray how a circle would be affected by very small increments of deformation

A

instantaneous strain ellipse

37
Q

in coaxial deformation how is (s1.) related to (s1) and (s3.) to (s3)

A

they are parallel

38
Q

in non coaxial deformation how are (s1.) and (s1) related and (s3.) and (s3)

A

S1 is successively rotated out of parallelism with (s1.) same with (s3.) and (s3)

39
Q

how does normal stress act on the surface

A

perpendicular

40
Q

how does shear stress act on the surface

A

parallel

41
Q

9 stresses

A

3 are normal

6 are shear