Discrepencies l.jpg
This presentation is the property of its rightful owner.
Sponsored Links
1 / 7

Discrepencies PowerPoint PPT Presentation


  • 86 Views
  • Uploaded on
  • Presentation posted in: General

Discrepencies. Different researchers use different cut-off points for what we term low-angle faults. We will go with the text definition of dips <30° Fault workers commonly refer to lenses in fault zones as horses when they are m-km scale structures

Download Presentation

Discrepencies

An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -

Presentation Transcript


Discrepencies l.jpg

Discrepencies

  • Different researchers use different cut-off points for what we term low-angle faults. We will go with the text definition of dips <30°

  • Fault workers commonly refer to lenses in fault zones as horses when they are m-km scale structures

  • Triangular features developed by erosion of fault surfaces on fault-bounded mountain fronts are fault facets. Flatirons are morphologically similar structures developed by erosion of tilted sedimentary layers


Finding fault s l.jpg

Finding fault(s)

How to evaluate whether a fault is present in the subsurface or an area of poor exposure


Fault but may be l.jpg

Abrupt lithologic change

Abrupt change in orientation of bedding or foliation

In both cases, look for evidence of fault-zone deformation with proximity to contact

Nonconformity - look for evidence such as basal conglomerate

Angular unconformity (see above) or Fold (look for lithologic continuity)

Fault….but may be


Use of stratigraphy l.jpg

Use of stratigraphy

  • Faults can cut out (omit) or stack (repeat) stratigraphic intervals. Stratigraphic omission or repetition can be evident through mapping or drill core.


Sense of slip in the absence of piercing points l.jpg

Sense of slip in the absence of piercing points

  • Relative ages of hanging wall and footwall materials constrains sense of slip

  • Metamorphic grade of hanging versus footwall constrains kinematics


Heterogeneity and anisotropy l.jpg

Heterogeneity and anisotropy

  • Fractures typically nucleate on heterogeneities (e.g., fossil)

  • Low-angle reverse, or thrust, faults localize in mechanically weak layers such as shale and evaporite. They cut across stronger layers in short steps

  • As long as it is favorably oriented, it is apparently energetically easier to reactivate an existing fault than create a new one


Pattern has meaning l.jpg

Pattern has meaning

  • Large-scale fault patterns reflect tectonic environments (plate movements)

  • Patterns reflect most energetically favorable response to imposed displacement

  • We will look at overall strains and patterns of faulting in a different order than indicated in syllabus: extensional, transcurrent, then contractional regimes


  • Login