of rocks [l17 p. 363-373 /ip-b] deformation of rocks [l17 p. 363-373 /ip-b]
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DEFORMATION OF OF ROCKSROCKS
[L17 P. 363-373 /IP-B][L17 P. 363-373 /IP-B]
Deformation of Deformation of rocksrocks
• Folds and faults are geologic structures.
• Structural geology - the study of the forces that deform rocks (stress applied) and the effects of this force (strain).
Phil Dombrowski Fig. 10.1
Small-scale Folds
Small-scale Faults
Tom Bean Fig. 10.2
StressStress(force per unit area)(force per unit area)
Types of directed (or differential ) stresses include:
• Compression - shorten
• Extension - elongate
• Shear - distort shape
Differential stress
StrengtStrengthh• Ability of an object to resist deformation
(low pressure vs. high pressure)
StraiStrainnis any change in original shape or
size of an object in response to stress acting on the object
Types of deformationTypes of deformation
• Elastic
• Ductile (plastic)
• Brittle (rupture)
Elastic deformationElastic deformation
Temporary change in shape or size that is recovered when the deforming force is removed
Think “rubber band”
Ductile (plastic) deformationDuctile (plastic) deformation• Permanent change in
shape or size that is not recovered when the stress is removed
• Occurs by the slippage of atoms or small groups of atoms past each other in the deforming material, without loss of cohesion
• Think “deck of cards”
Brittle deformation Brittle deformation (rupture(rupture))
• Loss of cohesion of a body under the influence of deforming stress
• Sucker breaks!!!
• Usually occurs along sub-planar surfaces that separate zones of coherent material
Typical stress and
strain curve
Factors that affect deformationFactors that affect deformation
• Temperature
• Pressure
• Strain rate
• Rock type
The variation of these factors determines if a rock will fault or fold.
Effects of rock type on deformationEffects of rock type on deformation
Some rocks are stronger than others.
competentcompetent:: rocks that deform only under great stresses
incompetentincompetent:: rocks that deform under moderate to low stresses
Effects of deformation on rock type Effects of deformation on rock type Experimental Deformation of Marble
M.S. Patterson
Fig. 10.7
Brittle Deformation (Under low pressure) Ductile Deformation
(Under high pressure)
Orientation of deformed rocks Orientation of deformed rocks
ATTITUDEATTITUDE - way to describe the orientation of geologic structures.
StrikeStrike: (compass) bearing of a line defined by the intersection of the plane in question and the horizontal
DipDip: acute angle between the plane and the horizontal, measured perpendicular to strike.
Fig. 10.4
Fig. 10.4
Dipping Sedimentary Beds
Chris Pellant Fig. 10.3
P.L. KresanP.L. Kresan
Cockscomb Ridge, S. Utah
Cockscomb Ridge, S. Utah
Dip
Strike
P.L. Kresan
Tectonic Forces and Resulting Tectonic Forces and Resulting DeformationDeformation
Fig. 10.6
BRITTLE DEFORMATION
A. Abrupt movement breaks or cracks strata
B. 2 kinds of breaks:
– 1. JOINTS - NO movement of blocks
– 2. FAULTS - YES movement of blocks
1. Movement along STRIKE
2. Movement along DIP
Columns Formed by
Joint-controlled
Weathering
Terry Englander Fig. 10.20
Joint-controlled Landscape, S.E. Utah
FaultsFaultsFractures in rocks created byearthquakes that have moved
A. Dip-slip faultsnormal
reverse
thrust
B. Strike-slip faults
right lateral or left lateral
Hanging-wall and footwall
Dip-slip faultsDip-slip faults
Motion of the fault blocks, parallel to the dip direction.
Classification of FaultsClassification of Faults
hanging wall
footwall
cross section
Normal Normal FaultFault
footwall
hanging wall
cross section
Normal Dip-slip Fault
Reverse FaultReverse Fault
footwall
hanging wall
cross section
Reverse Dip-slip Fault
Drape Fold over Reverse Fault, WY
George Davis
Thrust FaultThrust Fault
footwall
hanging wall
cross section
Thrust faults are low-angle reverse faults.
Thrust fault
Keystone Thrust Fault, S. Nevada
John S..Shelton
Cambrian Limestone
Jurassic Sandstone
Lewis Thrust,
Sawtooth Range,
Wyoming
Kurt N. Coonstenius
French Thrust, Wyoming
Cretaceous Shale
MississippianLimestone
Kurt N. Coonstenius
Strike-slip faultsStrike-slip faults
Motion of the fault blocks is parallel to the strike direction.
To determine the direction of strike, put toes on the fault line & look at the direction the opposite block moved.
Left-lateral Strike Slip FaultLeft-lateral Strike Slip Fault
map view
Right-lateral Strike Slip Right-lateral Strike Slip FaultFault
map view
Gudmundar E. Sigvaldason
Strike-slip Fault
Rift Valley Formed by ExtensionRift Valley Formed by Extension
Graben
Horst
Horst
Wildrose Graben, Southern California
NASA/TSADO/Tom Stack
1872 Fault Scarp, Southern California
1988 Armenian Earthquake Fault Scarp
Armando Cisternas
1992 Landers
Earthquake Fault Scarp
PLASTIC DEFORMATIONFOLDSFOLDS
anticlineanticline: older rocks on the inside
synclinesyncline: older rocks on the outside
(scale(scale - from mm to tens of km)
Fold TerminologyFold Terminology
Fig. 10.10
Symmetrical
Isoclinal
Asymmetrical
Overturned
RecumbentFig. 15.22
Bill Evarts
Axial plane
AnticlineAnticline
Fig. 10.11
Breck Kent
Asymmetric Folds
Phil Dombrowski Fig. 10.1
Overturned Folds
Overturned Syncline,
Israel
Geological Survey of Israel Fig. 10.13
Valley and Valley and Ridge Ridge
Province of Province of the the
Appalachian Appalachian MountainsMountains
Fig. 10.19
Valley and Ridge Province
P. L. Kresan
J. Shelton, Geology illustratedJ. Shelton, Geology illustrated Fig. 10.15
Plunging Folds in the Plunging Folds in the Valley and RidgeValley and Ridge
Raplee Anticline, S.E. Utah
Raplee Anticline on the San Juan River, Utah
Domes and BasinsDomes and Basins
Fig. 10.16
John S. Shelton Fig. 10.17
Sinclair Dome, Wyoming
Anticlines and SynclinesAnticlines and Synclines
Fig. 10.9
Geologic Geologic Map and Map and
Cross Cross SectionSection
Fig. 10.5
Outcrops of SynclineOutcrops of Syncline
Fig. 10.18
All pau