Faults Flashcards

1
Q

what is a fault

A

-a fracture (joint) or zone of fractures between two blocks of rock

-rock response to stresses, extensional, compressional and shear forces

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2
Q

difference between hanging wall and footwall

A

hanging wall is the block of rock above the fault line.

footwall is the block of rock below the fault line

(basically ground/ceiling)

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3
Q

types of faults

A

normal, reverse, strike-slip

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4
Q

what is a normal fault

A

-also known as dip-slip

defined by downwards movement of their hanging-walls, with respect to their footwalls.

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5
Q

how are normal faults formed

A

response to extensional forced

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6
Q

what is a reverse fault

A

-also known as thrust fault

defined by upwards movement of their hanging-walls
to footwalls.

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7
Q

how is a reverse fault formed

A

response to compressional forces

defined by upwards movement of hanging-walls to the footwalls

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8
Q

strike-slip fault

A

also known as sinistral/dexrel/wrench

rocks on either side of the fault are displaced along the strike of the fault surface dominantly

may be defined as sinistral (left-moving: right-bottom) or dextral (right-moving) dependent upon the direction of movement of one side compared to the other.

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9
Q

what is a fault plane

A

the flat surface of rock along which a geological fault occurs

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10
Q

dips of normal and reverse faults

A

average extensional faults dip:
60 degrees to the horizontal,

average reverse faults:
about 30 degrees to the horizontal

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11
Q

type of fault dips

A

-Planar faults
no systematic and progressive change in the angle of dip

locally dip may change significantly in relation to competency of strata but as a whole approximated straight line with depth average dip for the fault surface

Listric faults
get progressively shallower with depth. They may even become horizontal

know as ‘detachment’

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12
Q

what is strike

A

line formed by intersection of a horizontal plane and incline surface

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13
Q

type of fault strikes

A

Strike-parallel faults
concordant (towards) with the strike of the strata they cut

Dip-parallel faults
roughly perpendicular (discordant angled away) to the direction of strike of the strata they cut

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14
Q
A
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