strike and dip - inside minesinside.mines.edu/~cshorey/newfiles/lecture 13 - structure and...
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Structural Geology
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Strike and Dip• Strike is the direction of the line that is
formed by the intersection of the plane of the rock bed with a horizontal surface.
• Dip is the direction in which the steepest angle is formed between the plane of the rock bed and the horizontal surface.
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45
45
45
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I think that the red bed came first, then green, then yellow,
then black, then the whole sequence was tilted 45% to the
North.
N S
Common structural features
• Tilted beds• Joints• Faults• Folds• Boudinage
Stress and Strain• Stress is a force applied over a
volume of rock.–Compression, Tension, and Shear
• Strain is the deformation of a rock in response to stress.–Brittle, Ductile, and Elastic
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Here the strain is more akin to brittle as the cards slide past each other without deforming
GEOLOGIC STRUCTURES
Monoclinalfolds
Strike-slip (Transform) faults
Shear
BoudinageNormal faultsTension
FoldingReverse faults(Thrust faults)
Compression
ElasticDuctileBrittleSTRAINSTRESS
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Precambrian
Cretaceous
GEOLOGIC STRUCTURES
Monoclinalfolds
Strike-slip (Transform) faults
Shear
BoudinageNormal faultsTension
FoldingReverse and Thrust faults
Compression
ElasticDuctileBrittleSTRAINSTRESS
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GEOLOGIC STRUCTURES
Monoclinalfolds
Strike-slip (Transform) faults
Shear
BoudinageNormal faultsTension
FoldingReverse and Thrust faults
Compression
ElasticDuctileBrittleSTRAINSTRESS
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U
D
Slickensides
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GEOLOGIC STRUCTURES
Monoclinalfolds
Strike-slip (Transform) faults
Shear
BoudinageNormal faultsTension
FoldingReverse and Thrust faults
Compression
ElasticDuctileBrittleSTRAINSTRESS
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GEOLOGIC STRUCTURES
Monoclinalfolds
Strike-slip (Transform) faults
Shear
BoudinageNormal faultsTension
FoldingReverse and Thrust faults
Compression
ElasticDuctileBrittleSTRAINSTRESS
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GEOLOGIC STRUCTURES
JointsShear
JointsTension
JointsCompression
ElasticDuctileBrittleSTRAINSTRESS
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Continental Structure, Mountain Building and
Differentially Weathered Landforms
Shield or Craton is the stable interior of a continent characteristically composed of
ancient crystalline basement rock
Platform is the relatively horizontal undeformed sedimentary rocks onlapping the basement rock.
Figure 14.3
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Plutonic igneous Volcanic igneous
Sedimentary Metamorphic
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ISOSTACY
The floating of the Earth’s crust on the denser mantle so that vertical motions take place to achieve a balance between upward buoyancy and downward gravity.
3 ways mountains can form.
1.Compressive belts2.Fault block3.Volcanic
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Figure 14.C
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Figure 14.12AB Appalachian Orogeny
Figure 14.12CD
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Figure 14.12DE Figure 14.12F
Figure 14.13
Figure 14.15AB Cordilleran Orogney Figure 14.16
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Terranes are foreign pieces of land pasted on to the edge of a continent.
Usually start of as ocean islands.
Figure 14.11
Fault-block mountains• Mountains can also be formed by the
extension of the Earth’s crust.• Produces Horst and Graben topography
in which the higher Horsts become mountains.
• Grand Teton mountains in Wyoming are a prime example of this type of mountain.
Figure 14.18
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Epeirogeny and landforms• Epeirogenic movements are gradual
upward or downward movements of the continental crust.
• Occur with little deformation.– Minor tilting and slight faulting.
• Can still produce spectacular landforms when uplift occurs due to downcutting of stream systems and differential weathering.
Flatirons and Hogbacks
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Cuestas
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Mass Wasting• Shear stress vs. Shear strength• Shear stress created by gravity pulling
on a slope– Controlled by mass and slope
• Shear strength provided by the internal friction within the slope material
Safety factor (S.F.)• S.F.=shear stress/shear strength• S.F.<1
– Shear stress<<Shear strength --> stable• S.F.=1
– Shear stress=Shear strength --> slope failure
Slope Stabililty• Mass and slope• Climate, Vegetation• Water (groundwater)• Materials
– Rock type, sediment (fine vs. coarse), soil.
Classification of Mass Wasting
• RATE of MOVEMENT–Extremely slow (~1mm/year) to very
rapid (>100 km/hour)
• MATERIAL IN MOTION–Bedrock–Debris- (“soil”, sediment)
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Types of movement:• Flows - materials mix together
– creep, mud, debris, avalanche
•• Slides Slides -- coherent blocks/unitscoherent blocks/unitstranslationaltranslationalrotationalrotational
• Falls - free falling
Classification of Mass Wasting
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Types of movement:• Flows - materials mix together
– creep, mud, debris, avalanche• Slides - coherent blocks/units
translationalrotational
•• Falls Falls -- free fallingfree falling
Classification of Mass Wasting
Controlling Factors
• Slope angle• Local relief• Thickness of debris over bedrock• Planes of weakness ( in bedrock)
–bedding planes; foliation; joints–parallel to slope most dangerous
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Controlling Factors
• Climatic controls– Ice– Water– Precipitation– Vegetation
• Gravity– Shear force– Normal force– Shear strength
Controlling Factors• Water
–adds weight–increased pore pressure in saturated debris
decreases shear strength–water lubricates the material
• Triggering Mechanisms–Overloading–Undercutting–Earthquakes
Mass WastingTriggers:• Natural/transient
– Climate/Weather changes• Sudden increase in moisture
– Earthquakes• Anthropogenic
– Loading– Slope perturbation (excavation or filling)– Changes in water content
Human impact on mass wastingAddition of waterthrough irrigation, septic systems, artificial ponds or leaky in-ground pools, etc., loosens up slope material and adds weight, promoting slope failure
irrigation
pool or pond
septicsystem
Devegetation concentrates surface runoff and enhances erosion, resulting in steeper slopes. Reduced interception and evaporation increases amount of water in ground. (Also, construction of logging roads result in oversteepening.)
Preventing Landslides
• Preventing mass wasting of debris• Preventing rockfalls and rockslides on
highways
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Slope stabilization: keeping the water out
Drains and trenches keep water from infiltrating the
top of a slump
Short-term precaution against further water input and erosion
Revegetation and drainage