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StructureSolver StructureSolver
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  • Home
  • Learn More
    • Overview
    • Value Proposition
    • Interpretation
    • Structural Restoration
    • Structural Modeling
    • Area-depth Strain Analysis
    • Integrated Analysis
  • Petrel Plugin
    • Overview
    • Area-Depth Analysis in Petrel
    • Kinematic Structural Modeling in Petrel
    • Using Structural Components in Petrel
    • Transferring Interpretations Between Petrel And StructureSolver
    • Location and Measurement in StructureSolver
    • Plugin Workflow
  • Video Gallery
    • Structural Modeling Examples
      • Simple Extensional Growth Fault
      • Mississippi Canyon
      • NZ Crustal Fault
      • Failed Rift
      • Niger Delta Growth Fault
      • Lost Hills
      • Inversion Model
    • Structural Restoration Examples
      • Restore Section to Bathymetric Profile
      • Gulf of Mexico
      • NW Africa
      • Alberta Triangle Zone
    • Component Structural Restoration Examples
      • Toldado Anticline Component Restoration
      • Minibasin Component Restoration
      • Transform To Target
      • Salt Diapir Restoration
    • Area-Depth Graph Examples
      • Niger Delta Area Depth Analysis
      • Fault Trajectory Bermejo BasinFault Trajectory Bermejo Basin
      • Mapping Fault Shapes with Area-DepthMapping Fault Shapes with Area-Depth
    • Linked Modeling and Strain Analysis
      • Multiple Linked Structural Models
      • Niger Delta Fault Propagation
      • Multiple Thrust Fault Animation
      • Strain Modeling
    • Using StructureSolver:Basics
      • StructureSolver Interface
      • Context Menus
      • Interpretation Dashboard
      • Interpretation Basics
      • Annotation and Scale Bars
      • Getting Started with StructureSolver
      • Import from SEG-y File
      • Fault Terminations and Junctions
      • StructureSolver Solutions
      • Calibrating
      • Color Fill
    • Using StructureSolver: Structural Components
      • Component Creation and Management
      • Curve Transfer
    • Using StructureSolver: Restoration
      • Interpretation Guidelines
      • Interpretation Errors and Warnings
      • Vertical Shear Restoration
      • Flexural Slip Restoration
      • Inclined Shear Restoration
      • Restore Section Workflow
      • Restore Component Workflow
      • Rotate Section or Component
      • Add Vertical Shear Marker
      • Add Flexural Slip Horizon
      • Add Inclined Shear Marker
    • Using StructureSolver: Structural Modeling
      • Structural Modeling Basics
      • Adding Structural Surfaces to a Model
      • Structural Modeling Functions
      • Working with Multiple Structural Models
      • Structural Modeling Warnings and Errors
      • Trishear Basics
    • Using StructureSolver: Area-Depth Strain
      • Area-Depth Graph Basics
  • Case Studies
    • Bohai Bay Structural Modeling and Restoration
    • Mexican Ridges Presentation
    • Labrador Sea
    • Niger Delta - Quantitative Structural Analysis
    • Peru - Integrative Structural Analysis
  • Software
    • Current Release 8.0
    • Version 7.0
    • Version 6.0
    • Version 5.0
      • NewFeaturesV5.0
      • Color Fill
      • Component Creation and Management
      • Stretch and Shear
      • Transform To Target
      • Curve Transfer
      • Scale Bars
    • Release Notes
    • Technology Summary
    • Licensing and Pricing
  • Company
    • About us
    • Academic Outreach Program
    • Newsletters
  • Support
    • Software Support
    • Website Support

New Zealand Crustal Fault Structural Model

Video

Lock Hangingwall Cutoffs menu item was deprecated in Version 2.2. 

StructureSolver locks hangingwall cutoffs automatically as required and previous menu option has been removed. Hangingwall cutoffs are locked whenever a more surface is moved on the footwall side of the fault and whenever the bottom segment of a fault is modified in any way. This makes the modeling process much simpler and more intuitive. 

Discussion
This example illustrates how StructureSolver can be used to estimate the deep trajectory of crustal scale faults, using a relatively small amount of structural information from the cover section.  Such determinations can be valuable when doing basin-scale analysis. 
 
By varying the fault trajectory you can also get an estimate of the uncertainties in your solution.
 
Data courtesy Professor D. C. Lawton, University of Calgary (from New Zealand Government Technical Archives).
  • Simple Extensional Growth Fault
  • Mississippi Canyon
  • NZ Crustal Fault
  • Failed Rift
  • Niger Delta Growth Fault
  • Lost Hills
  • Inversion Model

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