stress and strain - city university of new york
TRANSCRIPT
![Page 1: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/1.jpg)
Faults
![Page 2: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/2.jpg)
BASIC DEFINITIONS► FAULT: A surface or narrow zone along which one side
has moved relative to the other. A fault may form through either brittle (fractures) or ductile (shear) deformation. Faults are classified based upon the orientation of the displacement vector along the fault surface.
DIP-SLIP FAULTS: Faults along which the movement is approximately parallel to the dip
STRIKE-SLIP FAULTS: Faults along which the movement is approximately parallel to the strike
OBLIQUE-SLIP FAULTS: Faults along which the movement is inclined to both the strike and dip of the fault surface. It may be described as the sum of a strike-slip and a dip-slip vector
![Page 3: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/3.jpg)
HANGING WALL vs FOOTWALL
► A fault divides rock into two fault blocks
► For any inclined fault, the block above the fault is the hanging wall block, and the block below the fault is the footwall block
www.data.scec.org/Module/footnt02.html
![Page 4: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/4.jpg)
CLASSIFICATION of DIP-SLIP FAULTS
► NORMAL FAULTS: Dip-slip faults on which the hanging wall moves down relative to the footwall
Place younger rocks on older rocks
May result in omission of strata
Form in regions of lateral extension
www.data.scec.org/
Module/footnt02.html
![Page 5: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/5.jpg)
EXAMPLES OFNORMAL FAULTS
Conjugate Normal Faults,
Canyonlands National Park
darkwing.uoregon.edu/~millerm/conjN1.html
Normal Fault Scarps, Turkey
www.msnucleus.org/.../pt/hazards/4/pth4_1a.html
Outcrop scale normal faults
![Page 6: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/6.jpg)
EXAMPLES OFNORMAL FAULTS
Conjugate Normal Faults,
Canyonlands National Park
darkwing.uoregon.edu/~millerm/conjN1.html
Normal Fault Scarps, Turkey
www.msnucleus.org/.../pt/hazards/4/pth4_1a.html
Outcrop scale normal faultsFW
HW
FWHW
FW
HW
FWHW
FWHW
![Page 7: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/7.jpg)
CLASSIFICATION of DIP-SLIP FAULTS
► THRUST or REVERSE FAULTS: Dip-slip faults on which the hanging wall moves up relative to the footwall
Place older rocks on younger rocks
May result in repetition of strata
Form in regions of lateral compression
www.data.scec.org/
Module/footnt02.html
![Page 8: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/8.jpg)
EXAMPLES OFTHRUST FAULTS
Thrust Fault in Concrete from 1964 Quake,
Anchorage, Alaska
www.ucmp.berkeley.edu/.../alaska/0709log.html
Thrust Fault in Sediments
www001.upp.so-net.ne.jp/fl-fg/05-01.htm
Outcrop scale thrust faultswww.pitt.edu/.../7Structures/ReverseFaults.html
![Page 9: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/9.jpg)
EXAMPLES OFTHRUST FAULTS
Thrust Fault in Concrete from 1964 Quake,
Anchorage, Alaska
www.ucmp.berkeley.edu/.../alaska/0709log.html
Thrust Fault in Sediments
www001.upp.so-net.ne.jp/fl-fg/05-01.htm
Outcrop scale thrust faultswww.pitt.edu/.../7Structures/ReverseFaults.html
FW
HW
FW
HW
FW
HW
![Page 10: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/10.jpg)
CLASSIFICATION of STRIKE-SLIP FAULTS
► RIGHT-LATERAL (DEXTRAL) FAULTS: Strike-slip faults across which the block moves to the right
► LEFT-LATERAL (SINISTRAL) FAULTS: Strike-slip faults across which the block moves to the right
![Page 11: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/11.jpg)
EXAMPLES OFSTRIKE-SLIP FAULTS
San Andreas Fault, CA
http://education.usgs.gov/california/
pp1515/chapter2/fig2-21.jpgRight Lateral Slip, Izmit, Turkey, 1999 Quake
http://www.geo.uib.no/jordskjelv/
index.php?topic=earthquakes&lang=en
Right Lateral Fault in Asphalt
www.uwsp.edu/.../fault_transform_photo.html
![Page 12: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/12.jpg)
EXAMPLES OFSTRIKE-SLIP FAULTS
San Andreas Fault, CA
http://education.usgs.gov/california/
pp1515/chapter2/fig2-21.jpgRight Lateral Slip, Izmit, Turkey, 1999 Quake
http://www.geo.uib.no/jordskjelv/
index.php?topic=earthquakes&lang=en
Right Lateral Fault in Asphalt
www.uwsp.edu/.../fault_transform_photo.html
![Page 13: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/13.jpg)
STRATIGRAPHIC INDICATORS OF FAULTS
►Truncation of Units
Unconformity? Intrusion?
►Omission of units
Unconformity?
►Repetition of Units
Folding?
![Page 14: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/14.jpg)
PHYSIOGRAPHIC INDICATORS OF FAULTS
► Scarps
Terraces? River Valley?
► Linear Valleys
Erodable Strata?
► Pull-Apart Basins or Push-Up Ridges
http://www.bedford.k12.ny.us/flhs/
science/images/sanandreas1.jpg
![Page 15: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/15.jpg)
MESOSCOPIC STRUCTURALINDICATORS OF FAULTS
► Slickensides
►Drag Folds
►Vein Sets
Horizontal Slickensideshttp://wso.williams.edu/~cgarvin/photos/
slickensides.jpg
Drag Fold Associated with Thrust Faultweb.umr.edu/.../205-mile_landslides.htm
![Page 16: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/16.jpg)
MESOSCOPIC STRUCTURALINDICATORS OF FAULTS
► Slickensides
►Drag Folds
►Vein Sets
Horizontal Slickensideshttp://wso.williams.edu/~cgarvin/photos/
slickensides.jpg
Drag Fold Associated with Thrust Faultweb.umr.edu/.../205-mile_landslides.htm
![Page 17: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/17.jpg)
Why do certain types of faults have
predictable dips?
![Page 18: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/18.jpg)
FRACTURE EXPERIMENTS
►To understand the mechanics of fracturing, geologists perform controlled experiments on rock cores
►Rock is wrapped in a metal jacket
Provides confining pressure
σ2 and σ3 are perpendicular to core length
► Piston presses along the length of the core
σ1 is parallel to core length
![Page 19: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/19.jpg)
FRACTURE EXPERIMENTS
► Core fractures with a consistent pattern
![Page 20: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/20.jpg)
FRACTURE EXPERIMENTS
► Core fractures with a consistent pattern
► Two sets of fractures with an acute angle of approximately 60º between them
Conjugate fractures
![Page 21: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/21.jpg)
FRACTURE EXPERIMENTS
► Core fractures with a consistent pattern
► Two sets of fractures with an acute angle of approximately 60º between them
Conjugate fractures
►σ1 bisects the acute
angle between the conjugate fractures
σ1
σ1
![Page 22: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/22.jpg)
FRACTURE EXPERIMENTS
►σ1 bisects the acute angle between the conjugate set
►σ3 bisects the obtuse angle between the conjugate set
►σ2 runs parallel to the intersection of the conjugate set
σ1
σ1
σ3
![Page 23: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/23.jpg)
ANDERSON’S THEORY OF FAULTING
►The surface of Earth is a “free surface”, that is, it is a surface that cannot support shear stress Shear stress = 0
► Shear stress = 0 along principal stress planes Principal stress directions must be parallel or
perpendicular to a principal stress plane
►The surface of Earth is a principal stress plane At the surface of Earth, the principal stress directions
must be parallel or perpendicular to a principal stress plane
![Page 24: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/24.jpg)
COMBINING FRACTURE EXPERIMENTS WITH
ANDERSON’S THEORY
►σ1 must be either parallel or perpendicular to Earth’s surface
► Fractures form in conjugate sets around σ1
►The orientation of fractures (faults) will vary with the orientation of σ1 and the other principal stresses
►There are only 3 possible orientations of the principal stresses relative to the Earth’s surface
![Page 25: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/25.jpg)
σ1 Vertical…
► Produces fractures/faults that dip at 60º
►Motion is along dip with hanging-wall down
►NORMAL FAULTS
![Page 26: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/26.jpg)
σ1 Horizontal, σ3 Vertical…
► Produces fractures/faults that dip at 30º
►Motion is along dip with hanging-wall up
►THRUST FAULTS
![Page 27: Stress and Strain - City University of New York](https://reader033.vdocuments.us/reader033/viewer/2022042318/625c6fb1f70cea499c0a6cc3/html5/thumbnails/27.jpg)
σ1 Horizontal, σ2 Vertical…
► Produces fractures/faults that dip at 90º
►Motion is along strike
► STRIKE-SLIP FAULTS