STRUCTURAL GEOLOGY HATCHER 11 Flashcards

1
Q

Belt of thrust faults occuring between underformed craton and metamorphic core of nearly every mountain

A

Foreland Fold-Thrust Belt

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2
Q

Zones of weak rocks (shale , coal or strong unit suscpetible to strain softening) where thrusts generaly propagates. French for “Ungluing”

A

Detachment or Decollements or Bedding thrusts

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3
Q

A high angle segment which may exist where thrust cuts across a strong unit from one detachment to another

A

Ramp (High Angle Decollement)

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4
Q

Thickness of strong units

A

Strut

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5
Q

Formed by faulting the CONNECTING LIMB of a anticline and syncline pair overthrowing the haging wall anticline and preserving footwall syncline

A

Break Thrust/Fold Thrust

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6
Q

A Break Thrust formed independently of folding but not having a footwall syncline

A

Shear Thrust/Fracture Thrust

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7
Q

Formed as the THRUST SURFACE CHANGES from steeper dip to shallower in an up-dip direction (Surface)
Steeply dipping sa ilalim tapos biglang naging gentle sa ibabaw *Hanging wall anticline NO FOOT WALL Syncline

Nagchange lang yung steepnes ng dip and nagterminate sa surface

A

Fault Bend Fold
(ShearThrust/Fracture Thrust)

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8
Q

Formed as layers of a Sed Sequence fold during propagation of thrust (Hanging Wall Anticline plus Footwall Syncline

Nagfold yung sed layers nung nag thrust faulting nagterminate sa fault ramp

A

Fault Progation Fold
(Break Thrust/Fold Thrust)

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9
Q

Fault Bend Fold: Shear Thrust: Fault Propagation fault:

A

Break Thrust

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10
Q

Folds that form near the thrust sruface due to friction wherein the footwall are deformed to synclines and the hanging wall to antilines

A

Drag Folds

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11
Q

Materials that have been grinded due to faulting and may be transported within the fault zone under the thrust sheet

Mga fragments of rocks or asperities na naerode due to faulting at natrap sa gitna ng footwall and hanging wall

A

Horses (Hanging Wall Fragments)

Slices (Footwall Fragmets)

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12
Q

Whats the age of the horses?

A

intermediate between the ages of the hanging and footwall

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13
Q

Smaller faults in a group of thrust faults

A

Imbricate Thrusts

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14
Q

Series of thrusts making up the entire foreland thrust belt

A

Imbricate Zone

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15
Q

Strutures bounded by two thrust fault of approx equal displacement separated by deformed interval that is thin relative to its total area and the Upper an Lower Master fault connected by imricates

A

Duplex

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16
Q

Upper Master fault

A

Roof Thrust

17
Q

Lower Master Fault

A

Floor Thrust

18
Q

Line of intersection of two fault surfaces

A

Branch Line

19
Q

A thrust that terminates at the surface

A

Erosion or Emergent Thrust

20
Q

A thrust that was aborted within the sedimentary section and never reached the surface

A

Blind Thrust

21
Q

Ends of thrust sheets that terminate in strike slop faults

A

Tear Faults

22
Q

When there’s a hole in the thrust sheet/hanging wall formed during folding, the footwall rocks are exposed surrounded by steeply dipping haging wall rocks such hole is called

A

Simple window or Fenster

23
Q

An erosional feature formed by renewed movement in an foled thrust sheet which creates an opening along the fault surface and will appear to be partly closed because the elongate outcrop pattern prallels tha fault trace

A

Eyelid Windows

24
Q

If an exposed footwall is exposed surrounded by the rocks of the hanging wall and the contact is an unconformity it is called

A

Inlier

25
Q

Disemembered part of a thrust sheet (Iniwan at nahiwalay na part ng thrust sheet).
Erosional Outliers

A

Klippe

26
Q

Larger separated remnant of a thrust sheet

A

Allochton

27
Q

Thrusts that involves transport of basement metamorphic and igneous rocks or both as part of the thrust sheet (Hanging Wall)

A

Crystalline Thrust