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Geology 3120 - Geology 3120 - Introduction to Strike-Slip Introduction to Strike-Slip Faults Faults
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Geology 3120 - Introduction to Strike-Slip Faults

Jan 23, 2016

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Geology 3120 - Introduction to Strike-Slip Faults. Levant Strike-Slip Faults. Outline. Stick-Slip and Creep Andersonian Theory Kinematics Strike-Slip Faults on Continental Margins Strike-Slip Faults on Mid-Ocean Ridges. Stick-Slip: Elastic Rebound Theory. D. Elastic Rebound Theory. - PowerPoint PPT Presentation
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Page 1: Geology 3120 -  Introduction to Strike-Slip Faults

Geology 3120 - Geology 3120 - Introduction to Strike-Slip FaultsIntroduction to Strike-Slip Faults

Page 2: Geology 3120 -  Introduction to Strike-Slip Faults

Levant Strike-Slip FaultsLevant Strike-Slip Faults

Page 3: Geology 3120 -  Introduction to Strike-Slip Faults
Page 4: Geology 3120 -  Introduction to Strike-Slip Faults
Page 5: Geology 3120 -  Introduction to Strike-Slip Faults

OutlineOutline

• Stick-Slip and Creep

• Andersonian Theory

• Kinematics

• Strike-Slip Faults on Continental Margins

• Strike-Slip Faults on Mid-Ocean Ridges

Page 6: Geology 3120 -  Introduction to Strike-Slip Faults

Stick-Slip: Elastic Rebound TheoryStick-Slip: Elastic Rebound Theory

Page 7: Geology 3120 -  Introduction to Strike-Slip Faults

Elastic Rebound TheoryElastic Rebound Theory

• Imagine a fence across an active Imagine a fence across an active

faultfault

Page 8: Geology 3120 -  Introduction to Strike-Slip Faults

Elastic Rebound TheoryElastic Rebound Theory

• Imagine a fence across an active Imagine a fence across an active

faultfault

• Regional deformation occurs but Regional deformation occurs but

the fault does not break. The the fault does not break. The

fence becomes curved.fence becomes curved.

Page 9: Geology 3120 -  Introduction to Strike-Slip Faults

Elastic Rebound TheoryElastic Rebound Theory

• Imagine a fence across an active Imagine a fence across an active

faultfault

• Regional deformation occurs but Regional deformation occurs but

the fault does not break. the fault does not break.

•Once the fault breaks, the fence Once the fault breaks, the fence

is sheared in half and marks offsetis sheared in half and marks offset

•Note that far-field strain may limit Note that far-field strain may limit

whether the fault accommodates whether the fault accommodates

all the plate motion at its traceall the plate motion at its trace

Page 10: Geology 3120 -  Introduction to Strike-Slip Faults

Elastic Rebound TheoryElastic Rebound Theory

Page 11: Geology 3120 -  Introduction to Strike-Slip Faults

Elastic Rebound TheoryElastic Rebound Theory

QuickTime™ and aCinepak decompressorare needed to see this picture.

Page 12: Geology 3120 -  Introduction to Strike-Slip Faults

Creep (Aseismic Slip)Creep (Aseismic Slip)

• Imagine a fence across an active Imagine a fence across an active

faultfault

• Slip occurs slowly on the fault Slip occurs slowly on the fault

continually over time.continually over time.

• Creeping faults do not store Creeping faults do not store

elastic energy that might be elastic energy that might be

released by a stick-slip event (an released by a stick-slip event (an

earthquake)earthquake)

Page 13: Geology 3120 -  Introduction to Strike-Slip Faults

Andersonian TheoryAndersonian Theory

Page 14: Geology 3120 -  Introduction to Strike-Slip Faults

Conjugate Strike-Slip Conjugate Strike-Slip

FaultsFaults

Page 15: Geology 3120 -  Introduction to Strike-Slip Faults

Determining Sense of SlipDetermining Sense of Slip

Page 16: Geology 3120 -  Introduction to Strike-Slip Faults

Right-Lateral (Dextral)Right-Lateral (Dextral)

Page 17: Geology 3120 -  Introduction to Strike-Slip Faults

Left-Lateral (Sinistral)Left-Lateral (Sinistral)

Page 18: Geology 3120 -  Introduction to Strike-Slip Faults

Arrow Heads ( ) and Tails ( )Arrow Heads ( ) and Tails ( )

Block moving toward you like an arrowhead Block moving toward you like an arrowhead

heading towards youheading towards you

Block moving away from you like seeing the Block moving away from you like seeing the

feathers of an arrow feathers of an arrow

Page 19: Geology 3120 -  Introduction to Strike-Slip Faults

Arrow Heads ( ) and Tails ( )Arrow Heads ( ) and Tails ( )

Right-lateral or left-lateral?Right-lateral or left-lateral?

Page 20: Geology 3120 -  Introduction to Strike-Slip Faults

Arrow Heads ( ) and Tails ( )Arrow Heads ( ) and Tails ( )

Left-lateralLeft-lateral

Page 21: Geology 3120 -  Introduction to Strike-Slip Faults

Arrow Heads ( ) and Tails ( )Arrow Heads ( ) and Tails ( )

Sinistral or Dextral?Sinistral or Dextral?

Page 22: Geology 3120 -  Introduction to Strike-Slip Faults

Arrow Heads ( ) and Tails ( )Arrow Heads ( ) and Tails ( )

DextralDextral

Page 23: Geology 3120 -  Introduction to Strike-Slip Faults

Strike-Slip Faulting: Shallow Brittle vs Deep Strike-Slip Faulting: Shallow Brittle vs Deep

ShearShear

Page 24: Geology 3120 -  Introduction to Strike-Slip Faults

Strike-Slip Faulting: EQ’s = dislocationsStrike-Slip Faulting: EQ’s = dislocations

See http://www.data.scec.org/Module/links/landrupt.html

Landers rupture propagation movies

Page 25: Geology 3120 -  Introduction to Strike-Slip Faults

Strike-Slip Faults on Continental Strike-Slip Faults on Continental

MarginsMargins

What is the sense of slip?What is the sense of slip?

N50 m

Page 26: Geology 3120 -  Introduction to Strike-Slip Faults

Strike-Slip Faults on Continental Strike-Slip Faults on Continental

MarginsMargins

Right-lateral (dextral)Right-lateral (dextral)

N50 m

Page 27: Geology 3120 -  Introduction to Strike-Slip Faults

TranstensionTranstension

Page 28: Geology 3120 -  Introduction to Strike-Slip Faults

Development of a Pull-Apart Development of a Pull-Apart

BasinBasin

Page 29: Geology 3120 -  Introduction to Strike-Slip Faults

Pull-Apart BasinPull-Apart Basin

Page 30: Geology 3120 -  Introduction to Strike-Slip Faults

Initial Releasing BendInitial Releasing Bend

Page 31: Geology 3120 -  Introduction to Strike-Slip Faults

Evolution of a Releasing Evolution of a Releasing

BendBend

Page 32: Geology 3120 -  Introduction to Strike-Slip Faults

Normal (-) Flower Structure - Normal (-) Flower Structure -

Tulip Tulip

Page 33: Geology 3120 -  Introduction to Strike-Slip Faults

TranspressionTranspression

Page 34: Geology 3120 -  Introduction to Strike-Slip Faults

Development of a Restraining Development of a Restraining

BendBend

Page 35: Geology 3120 -  Introduction to Strike-Slip Faults

Initial Restraining BendInitial Restraining Bend

Page 36: Geology 3120 -  Introduction to Strike-Slip Faults

Evolution of a Restraining Evolution of a Restraining

BendBend

Page 37: Geology 3120 -  Introduction to Strike-Slip Faults

Reverse (+) Flower Structure - Reverse (+) Flower Structure -

PalmPalm

Page 38: Geology 3120 -  Introduction to Strike-Slip Faults

Summary of Flower Structures - Palms Summary of Flower Structures - Palms

& Tulips& Tulips

Page 39: Geology 3120 -  Introduction to Strike-Slip Faults

Oceanic Strike Slip fault: TransformsOceanic Strike Slip fault: Transforms

Page 40: Geology 3120 -  Introduction to Strike-Slip Faults

Strike-Slip Faults on Mid-Ocean Strike-Slip Faults on Mid-Ocean

RidgesRidges

What is the sense of slip?What is the sense of slip?

Page 41: Geology 3120 -  Introduction to Strike-Slip Faults

Strike-Slip Faults on Mid-Ocean Strike-Slip Faults on Mid-Ocean

RidgesRidges

Right-lateral (Dextral)Right-lateral (Dextral)

Page 42: Geology 3120 -  Introduction to Strike-Slip Faults

Pacific-Antarctic RidgePacific-Antarctic Ridge

Magnetic anomalies from present to 9.9 MaMagnetic anomalies from present to 9.9 Ma

Warm colors indicate positive polarityWarm colors indicate positive polarity

Cool colors indicate reverse polarityCool colors indicate reverse polarity