STRUCTURAL GEOLOGY
Structural Geology
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What is Structural Geology
Deals with form, arrangement, and internal structure of rocks, especially
the description representation, and analysis of structures
Review
Stress, Strain, Rupture
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Types of Pressure
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Confining pressure (Confining stress)
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Directed pressure - Stress
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tension - pull apart
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compression -push together
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shear - scissor action
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How do rocks respond to stress?
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Strain - deformation - elastic
and plastic
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Brittle fracture - rupture, breakage
Earthquakes
How do rocks respond
to stress?
Stress and Strain
Structural Geology
Rock Behavior
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Rock Behavior - ductile vs. brittle
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Ductile - rocks bend, fold; get
ductile behavior:
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at higher temperature
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at higher confining pressure
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if rocks contain water
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if stress is applied over long period of time
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depending on nature of the material
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shale more ductile than limestone

Laboratory Experiments with Marble
Folds
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bending of horizontal features
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common with layered rock
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occur on a scale of mm to km
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"tightness" varies depending on
deformation
Folds (cont.)
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How does a geologist recognize
folds in the field?
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see an outcrop
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measure orientation of beds and
infer from changes in orientation
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Measuring bed orientation
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orientation of 3 points relative
to horizontal plane, or
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Strike and dip
Strike and Dip
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Strike - orientation of a line
formed by the intersection of the bed with the horizontal plane
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Dip - angle between horizontal
plane and bed
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note: dip direction will be at right angles
to strike
Folds
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Cross-section and map-view of fold,
with strikes and dips marked
Geologic Map
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Colors distinguish different formations
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Ex: Purple - Cook Mountain Formation
Characterizing Folds (cont.)
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Fold Anatomy
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Axial Plane - surface which divides
a fold as symmetrically as possible
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Hinge line may plunge into the
earth (plunging fold)
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Plunge - angle of hinge line to
horizontal plane
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Trend - compass orientation of
line

Characterizing Folds
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Syncline
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Younger beds in core of fold
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Often "U"-shaped, but not always
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Anticline
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Older beds in core of fold
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Often "A"-shaped, but not always
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Monocline
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step-like bend in an otherwise gently dipping
or horizontal bed
Characterizing Folds (cont.)
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Other types of folds
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Asymmetrical
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Overturned
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Limb tilted more than 90º from horizontal
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Recumbent
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Axial plane horizontal, or nearly horizontal
Characterizing Folds
Summary
Characterizing Folds (cont.)
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Other Features
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Domes - circular or elliptical
anticline (Ex: Black Hills, SD)
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Basin - circular or elliptical
syncline (Ex: Michigan Basin)
Joints and Faults
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Products of brittle behavior
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Joint - fracture in rock
along which no appreciable relative displacement has occurred
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Fault - fracture in rock along
which there has been displacement.
Joints
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Joints
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may be due to compression, tension or shear stress
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tension joints form a regular pattern at right
angles to tension
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joints occur in sets, not alone
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Joint sets have a common origin
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usually consist of parallel joints
Faults
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Faults - must be able to prove
displacement for a fracture to be a fault
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Evidence of faulting
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crushed rock in fracture
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fault breccia
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mylonite - fine grained, recrystallized
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fault gouge - fine grained, soft
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slickenslides - polished and striated
surfaces, formed by friction
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Displacement of bed (or man-made feature like
a fence)
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Fault drag (drag folding) - folding due to drag
on a bed
Faults (cont.)
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Types of Faults
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Dip-slip - displacement up or down
dip of fault plane

Dip-slip Faults
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Normal fault - hanging wall block
moves down; tension
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Reverse fault - hanging wall block
moves up; compression
Normal or Reverse fault?
Dip-Slip (cont.)
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Thrust fault (Fig. 12-18) - low
angle reverse fault
Strike-slip Faults
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Strike-slip - displacement parallel
to strike of fault plane; movement is horizontal
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Left lateral fault
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Right lateral fault
Faults (cont.)
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oblique-slip - displacement is
a combination of dip-slip and strike-slip motion
Faults and Plate Boundaries
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Divergent
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Convergent (Subduction zones)
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compression
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reverse and thrust faulting
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Transform