Earthquake Engineering - Vol 2 | 21. Geological Faults by Abraham | Learn Smarter
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21. Geological Faults

Geological faults are critical fractures in the Earth's crust that play a significant role in earthquake dynamics. The chapter discusses the definition, causes, and classifications of faults, along with their geometrical and mechanical properties. It emphasizes the importance of understanding faults for effective civil engineering practices, especially regarding risk assessment and infrastructure planning in seismically active regions.

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Sections

  • 21

    Geological Faults

    Geological faults are fractures in the Earth's crust that play a critical role in seismic activity, influencing earthquake engineering and infrastructure design.

  • 21.1

    Definition And Characteristics Of Faults

    Faults are geological fractures where displacement has occurred due to tectonic forces, critical for understanding earthquakes.

  • 21.2

    Causes Of Faulting

    Faulting occurs due to tectonic stresses, volcanic activity, crustal loading/unloading, and human activities.

  • 21.3

    Classification Of Faults

    Faults are classified based on the relative motion of rock masses and the orientation of the fault plane.

  • 21.3.1

    Based On Direction Of Displacement

    This section classifies geological faults based on the direction of displacement, highlighting dip-slip, strike-slip, and oblique-slip faults.

  • 21.3.1.a

    Dip-Slip Faults

    Dip-slip faults involve vertical movement of rock layers along the fault plane, with normal and reverse faults as the primary types.

  • 21.3.1.b

    Strike-Slip Faults

    Strike-slip faults are characterized by horizontal movement along their fault plane, where the opposing sides slide past each other.

  • 21.3.1.c

    Oblique-Slip Faults

    Oblique-slip faults involve both vertical and horizontal displacement of rock masses along fault planes.

  • 21.4

    Fault Geometry And Terminology

    This section covers the essential concepts and terminology related to fault geometry, which is crucial for understanding fault behavior and seismic potential.

  • 21.5

    Fault Mechanics And Stress Analysis

    This section discusses the mechanics of faults under stress, outlining the Mohr-Coulomb failure criterion and its significance in understanding fault behavior and seismic activity.

  • 21.6

    Active, Inactive, And Reactivated Faults

    This section defines and categorizes faults into active, inactive, and reactivated, highlighting their significance in geological studies and earthquake preparedness.

  • 21.7

    Mapping And Identification Of Faults

    This section discusses various techniques used to map and identify geological faults, which are crucial for understanding seismic hazards.

  • 21.8

    Faults And Earthquake Generation

    This section explains how faults serve as zones of weakness where stress accumulation leads to earthquakes through mechanisms such as the Elastic Rebound Theory.

  • 21.9

    Fault Hazard Assessment And Risk Mitigation

    This section discusses the critical methods employed by civil engineers to assess faults' seismic risks and implement risk mitigation strategies.

  • 21.10

    Important Fault Systems In India

    This section outlines key fault systems in India, highlighting their significance in seismic activity and national hazard mapping.

  • 21.11

    Engineering Implications Of Faults

    This section discusses the critical impact of geological faults on engineering practices, including foundation design, tunnel alignment, dam construction, and transportation infrastructure.

  • 21.12

    Fault Rupture Propagation And Seismic Waves

    This section details the mechanisms of fault rupture propagation and the types of seismic waves generated during earthquakes.

  • 21.13

    Fault Creep And Locked Faults

    This section discusses fault creep and locked faults, highlighting their behavior and significance in earthquake mechanics.

  • 21.14

    Fault-Induced Ground Deformations

    This section discusses the various permanent surface deformations caused by active faulting and their implications for civil engineering.

  • 21.15

    Blind Faults And Hidden Seismic Sources

    Blind faults are seismic sources that do not rupture the surface, posing significant risks during earthquakes due to their hidden nature.

  • 21.16

    Faults And Soil-Structure Interaction

    This section explores how faults influence interactions between soil and structural systems during seismic events.

  • 21.17

    Instrumentation And Monitoring Of Fault Activity

    The section discusses the importance of monitoring active faults for hazard mitigation, outlining the key instruments used in this process.

  • 21.18

    Engineering Case Studies Involving Faults

    This section explores significant engineering case studies related to faults, highlighting the impact of fault movements on infrastructure and the importance of incorporating fault data in engineering design.

  • 21.19

    Guidelines For Civil Engineers Regarding Fault Zones

    Civil engineers must consider fault zones in site selection, design, and zoning to mitigate seismic risks.

Class Notes

Memorization

What we have learnt

  • Faults are fractures in the...
  • Earthquake risk is associat...
  • Effective fault mapping and...

Final Test

Revision Tests