STRUCTURAL GEOLOGY HATCHER 9 Flashcards

1
Q

Plane of dispplacement or the actual movement surface

A

Fault plane

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2
Q

Rock mass resting on the fault plane

A

Hanging wall

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3
Q

Rock mass beneath the fault plane

A

Footwall

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4
Q

Movement parallel to the plane surface

A

Slip

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5
Q

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

A

Net Slip ot True Displacement

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6
Q

The net displacement of the combined Strike and Dip Slip

A

Rake

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7
Q

Heave and Throw are componets of

A

Dip Slip

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8
Q

Heave corresponds to

A

the horizontal component normal to the strike

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9
Q

Throw Corresponds to

A

the Vertical component

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10
Q

Polished fault SURFACES

A

Slickensides

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11
Q

STRIATIONS on such surfaces

A

Slickenlines

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12
Q

Aligned FIBROUS MINERALS on a movement surface

A

Slickenfibers

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13
Q

What are these three and their implication?

A

Lineations indicates relative movement along a surface

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14
Q

A british geologist who classified faults

A

Ernest Anderson

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15
Q

HW moved down relative to FW

A

Normal Fault

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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
Q

faults that that converge toward a single point

A

Radial fault

26
Q

Faults that are concentric around a single point

A

Concentraic Fault

27
Q

Fault: Assymetric Repetion= _______: Symmetric repetition

A

Fold

28
Q

produced along a fault when units appeared to be pulled INTO a Fault during movement

A

Drag (Eto ung line ng bedding magbebend towards the plane)

29
Q

In a thrust fault, a drag in the hanggin wall would look like

A

Being pulled down dip

30
Q

Drag in listric faults where layering appears to have been darg down dop parallel to the movement along the fault

A

Reverse drag

31
Q

Is slickensides and slickenlines enough to prove significant faulting?

A

No, they may forrm on bedding surfaces during folding or may actaully form on joints that have small shear displacement

32
Q

A topographic surface whch is offset by DIP SLIP motion along a fault and DIRECTLY INDICATE the MOVEMENT SENSE of a fault

A

Fault Scarp

33
Q

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

A

Fault Line Scarp

34
Q

A fault line scarp in which erosion preserves the movement semse

A

Resequent Fault Line scarp

35
Q

A fault line scarp that have been eroded and provides a fault movement sense

A

Obsequent Fault Line Scarp

36
Q

Primary Criteria

A

Repetition and Omission of Strat Units
Displacement of recognizable markers
Truncation on of earlier structure

37
Q

The observation that maximum principal stress bisects acute angle between the conjugate shear planes of the stress elipsoid

A

Hartman’s Rule

38
Q

Formula for acute angle between shear planes

A

angle = 45 - angle of internal friction/2