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Transform fault

  • Transform Faults Represent One of the Three

    Transform Faults Represent One of the Three

  • Chapter 2

    Chapter 2

  • Segmentation of Transform Systems on the East Pacific Rise

    Segmentation of Transform Systems on the East Pacific Rise

  • Reducing Risk Where Tectonic Plates Collide—A Plan to Advance Subduction Zone Science

    Reducing Risk Where Tectonic Plates Collide—A Plan to Advance Subduction Zone Science

  • Transform Continental Margins – Part 1: Concepts and Models Christophe Basile

    Transform Continental Margins – Part 1: Concepts and Models Christophe Basile

  • The Ocean Basin & Plate Tectonics

    The Ocean Basin & Plate Tectonics

  • Two Classes of Transform Faults

    Two Classes of Transform Faults

  • Plate Tectonics

    Plate Tectonics

  • Origin and Models of Oceanic Transform Faults

    Origin and Models of Oceanic Transform Faults

  • On the Thermal Structure of Oceanic Transform Faults 2 Mark D

    On the Thermal Structure of Oceanic Transform Faults 2 Mark D

  • Earth Hazards of The

    Earth Hazards of The

  • On the Segmentation of the Cephalonia–Lefkada Transform Fault Zone (Greece) from an Insar Multi-Mode Dataset of the Lefkada 2015 Sequence

    On the Segmentation of the Cephalonia–Lefkada Transform Fault Zone (Greece) from an Insar Multi-Mode Dataset of the Lefkada 2015 Sequence

  • Plate Boundaries

    Plate Boundaries

  • Nonlinear Viscoelasticity and the Formation of Transverse Ridges

    Nonlinear Viscoelasticity and the Formation of Transverse Ridges

  • Can Subduction Initiation at a Transform Fault Be Spontaneous? Diane Arcay 1, Serge Lallemand 1, Sarah Abecassis 1, and Fanny Garel 1 1Geosciences Montpellier, Univ

    Can Subduction Initiation at a Transform Fault Be Spontaneous? Diane Arcay 1, Serge Lallemand 1, Sarah Abecassis 1, and Fanny Garel 1 1Geosciences Montpellier, Univ

  • Tectonic Inheritance at a Continental Margin William A

    Tectonic Inheritance at a Continental Margin William A

  • Earthquake Slip on Oceanic Transform Faults

    Earthquake Slip on Oceanic Transform Faults

  • Serpentinized Peridotite Versus Thick Mafic Crust at the Romanche Oceanic Transform Fault Emma P.M

    Serpentinized Peridotite Versus Thick Mafic Crust at the Romanche Oceanic Transform Fault Emma P.M

Top View
  • Oceanic and Continental Transform Faults
  • Anatomy of Strike-Slip Fault Tsunami Genesis
  • Tsunami Hazards
  • Deterministic Tsunami Hazard Assessment of Sines - Portugal
  • A Passive Plate Margin Continental Margins Are Not Necessarily Plate Margins! Earthquake Locations
  • JA Tony Fallin Ltr. Re
  • Oceanic Fault Zones Reconstructed
  • 14. Some Aspects of Plate Tectonics in the Arabian Sea
  • Progressive Evolution of Step-Overs and Bends
  • Transform Margins: Development, Controls and Petroleum Systems – an Introduction
  • Can Subduction Initiation at a Transform Fault Be Spontaneous?
  • Aseismic Transient Slip on the Gofar Transform Fault, East Pacific Rise
  • Distinctive Seafloor Fabric Produced Near Western Versus Eastern
  • The Geophysics, Geology and Mechanics of Slow Fault Slip
  • Plate Tectonics
  • Oceanic Transform Fault Seismicity and Slip Mode Influenced by Seawater Infiltration
  • Evaluation of Tsunami Sources with the Potential to Impact the U.S. Atlantic and Gulf Coasts
  • Model a Spreading Ocean Floor Offset by Transform Faults a Model of the Transform Fault ‘Steps’ in Oceanic Ridges and Their Magnetic Stripes


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