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Related Concept Videos

Fault Types01:18

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When analyzing a single line-to-ground fault from phase A to ground at a three-phase bus, it is important to consider the fault impedance. This impedance is zero for a bolted fault, equal to the arc impedance for an arcing fault, and represents the total fault impedance for a transmission-line insulator flashover. To derive sequence and phase currents, fault conditions are translated from the phase domain to the sequence domain.
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Complex fault interaction controls continental rifting.

John B Naliboff1,2, Susanne J H Buiter3,4, Gwenn Péron-Pinvidic3

  • 1Team for Solid Earth Geology, Geological Survey of Norway, Trondheim, 7040, Norway. jbnaliboff@ucdavis.edu.

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|October 31, 2017
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Summary
This summary is machine-generated.

Structural inheritance and changing extension velocities shape rifted margins. Early faults influence later evolution, creating distinct margin domains through complex interactions.

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Area of Science:

  • Geology
  • Tectonics
  • Geophysics

Background:

  • Rifted margins represent continental-oceanic transitions and record tectonic history.
  • Multiphase deformation creates distinct margin domains, but transition processes are unclear.

Purpose of the Study:

  • To investigate how structural inheritance and extension velocity variations control rifted margin architecture and evolution.
  • To elucidate the processes governing transitions between margin domains.

Main Methods:

  • High-resolution numerical simulations of continental rifting.
  • Modeling of crust and mantle lithosphere deformation.
  • Analysis of fault network evolution and reactivation.

Main Results:

  • Distinct margin domains form with increasing extension velocities over time.
  • Deformation concentrates along migrating, lithosphere-scale detachment faults.
  • Early-phase faults significantly control subsequent structural evolution and domain formation.

Conclusions:

  • Structural inheritance and extension velocity are key controls on rifted margin architecture.
  • Fault interaction processes, driven by early structures, create observed margin domains.
  • Numerical models provide detailed insights into rifted margin development.