Faults - Structural Geology - Lecture Slides, Slides of Geology

In these lecture slides, following are the main points that have been discussed : Fault, Bend Folding, Propagation Folding, Detachment Folding, Buckles, Multilayers, Trishear, Evaluating, Structural Style, Forelimb

Typology: Slides

2012/2013

Uploaded on 07/22/2013

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Faults and Faulting
Geol342
2008
Many diagrams are from Earth Structure, van der Pluijm and Marshak, 2004
Topics
Faults on outcrop, maps, and cross sections
Fault zones and fault rocks
Types of faults and terminology
Slip vs separation
Faults in wells
Fault propagation
Faults, fault zones, shear zones Terminology
Hanging wall
Foot wall
Fault Zone
in Granitic
Gneiss
Fault scarp after an earthquake- Nevada
Docsity.com
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1

Faults and Faulting

Geol

Many diagrams are from Earth Structure, van der Pluijm and Marshak, 2004 2008

Topics

  • Faults on outcrop, maps, and cross sections
  • Fault zones and fault rocks
  • Types of faults and terminology
  • Slip vs separation
  • Faults in wells
  • Fault propagation

Faults, fault zones, shear zones (^) Terminology

Hanging wall

Foot wall

Fault Zone in Granitic Gneiss

Fault scarp after an earthquake- Nevada

2

Plate Boundary-San Andreas Fault

Fault

Fence

Fault zone in Quartzites- Brooks Range

Small Normal Faults

Small Thrust Fault – Moss Beach, Ca

Types of fault

Oblique slip

4

Fault zone breccia in Quartzite Brooks Range, AK

Hydrothermal Fault Breccia

Fault Melt

Mylonites

Undeformed granite Deformed

Young Mountains-Active Fault –Basin and Range Province

5

Evolution of an Active Mountain Front

Triangular Facets on an active Mountain Front

Faults Symbols in Map View

Normal Faults

Thrust Faults

Decorations are on the hanging wall

Strike- slip

Fault on a Geological Map

What kind of fault is this? North

Map View of Faults Slip vs. Separation

7

Faults from well data

Faults are shear fractures in an elastic solid

Fault Propagation

  • Right-lateral Coulomb stress change on planes parallel to the main fault (Stein and Lisowski, 1983).

The longer a fault, the more displacement it has