STRUCTURAL GEOLOGY HATCHER 9 Flashcards

1
Q

Plane of dispplacement or the actual movement surface

A

Fault plane

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Rock mass resting on the fault plane

A

Hanging wall

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Rock mass beneath the fault plane

A

Footwall

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Movement parallel to the plane surface

A

Slip

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

the total amount of motion measured parallel to the direction of motion

A

Net Slip ot True Displacement

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

The net displacement of the combined Strike and Dip Slip

A

Rake

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Heave and Throw are componets of

A

Dip Slip

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Heave corresponds to

A

the horizontal component normal to the strike

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Throw Corresponds to

A

the Vertical component

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Polished fault SURFACES

A

Slickensides

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

STRIATIONS on such surfaces

A

Slickenlines

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Aligned FIBROUS MINERALS on a movement surface

A

Slickenfibers

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

What are these three and their implication?

A

Lineations indicates relative movement along a surface

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

A british geologist who classified faults

A

Ernest Anderson

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

HW moved down relative to FW

A

Normal Fault

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

two normal fault dipping TOWARDS ONE ANOTHER produces

A

Graben - dropped down block

17
Q

Two normal faults dipping away from each other

A

Horst - Up thrown block

18
Q

Normal faults that exhibit concave up geometry that is STEEP plane near the surface and gentler within depths

A

Listric Normal Fault or Lag

19
Q

Type of fault produced in conjuction with Listric Fault

A

Rollover Anticline

20
Q

HW moved up relative to FW

A

Reverse and Thrust Faults

21
Q

Age of Reverse Faults

A

45deg or greater (>45)

22
Q

Age of Thrust Faults

A

30deg or less (<30)

23
Q

Strike slip fault that compensates differences in Motion between plates

A

Transform Faults

24
Q

faults that are approximately parallel to one another unconnected but sometimes overlap

A

En Enchelon Fault

25
faults that that converge toward a single point
Radial fault
26
Faults that are concentric around a single point
Concentraic Fault
27
Fault: Assymetric Repetion= _______: Symmetric repetition
Fold
28
produced along a fault when units appeared to be pulled INTO a Fault during movement
Drag (Eto ung line ng bedding magbebend towards the plane)
29
In a thrust fault, a drag in the hanggin wall would look like
Being pulled down dip
30
Drag in listric faults where layering appears to have been darg down dop parallel to the movement along the fault
Reverse drag
31
Is slickensides and slickenlines enough to prove significant faulting?
No, they may forrm on bedding surfaces during folding or may actaully form on joints that have small shear displacement
32
A topographic surface whch is offset by DIP SLIP motion along a fault and DIRECTLY INDICATE the MOVEMENT SENSE of a fault
Fault Scarp
33
When such topographic surface has been eroded along the fault and have been lowered to the topographic surface which removes anuu resistant hanging wall and does not directly give the movement sense
Fault Line Scarp
34
A fault line scarp in which erosion preserves the movement semse
Resequent Fault Line scarp
35
A fault line scarp that have been eroded and provides a fault movement sense
Obsequent Fault Line Scarp
36
Primary Criteria
Repetition and Omission of Strat Units Displacement of recognizable markers Truncation on of earlier structure
37
The observation that maximum principal stress bisects acute angle between the conjugate shear planes of the stress elipsoid
Hartman's Rule
38
Formula for acute angle between shear planes
angle = 45 - angle of internal friction/2