Characterizing%20Fault%20Populations%20and%20Seismicity%20on%20an%20Active%20Plate%20Boundary%20Using%20GIS - PowerPoint PPT Presentation

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Characterizing%20Fault%20Populations%20and%20Seismicity%20on%20an%20Active%20Plate%20Boundary%20Using%20GIS

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Characterizing Fault Populations and Seismicity on an Active Plate Boundary Using GIS Tip Meckel Ph.D. Candidate Geological Sciences Outline Reasons for study The ... – PowerPoint PPT presentation

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Title: Characterizing%20Fault%20Populations%20and%20Seismicity%20on%20an%20Active%20Plate%20Boundary%20Using%20GIS


1
Characterizing Fault Populations and Seismicity
on an Active Plate Boundary Using GIS
  • Tip Meckel
  • Ph.D. Candidate
  • Geological Sciences

2
Outline
  • Reasons for study
  • The Macquarie Ridge Plate Boundary
  • Data Sets Involved in Study
  • GIS Project
  • Results and Significance
  • Conclusions

3
Why Study Plate Boundaries?
  • Seismic Hazard

Better understanding of tectonics is important!
Images courtesy of USGS unless noted otherwise
4
What are plate boundaries?
  • Basic concepts

5
The Macquarie Ridge Plate Boundary
  • Benefits of studying this boundary
  • Similar to San Andreas Boundary
  • It is completely naked!

6
Flying over the Macquarie Ridge!
Movie courtesy of the Australian Geological Survey
7
Why use GIS?
  • Interpretations rely heavily on maps
  • advantage to having data incorporated into map in
    table form
  • Spatial analysis of features and associated data

8
Data sets using
  • Entire Dissertation
  • Remotely Sensed Data from Ship Bathymetry,
    Sidescan Sonar, Gravity, Magnetics, and Seismic.
  • GIS Project
  • Line coverage of Faults interpreted on seafloor
  • Point coverage earthquake data from USGS
  • Bathymetry?

9
GIS Project
  • Import line drawing into Arc Format
  • Convert line drawing to ASCII and import
  • Thanks to Christina Massell and Chris McFarlane
  • Obtain USGS earthquake data and convert to a
    point coverage in correct latitude /longitude
    projection
  • Use data table to color earthquakes according to
    magnitude and depth

10
GIS Results I
11
GIS Results II
12
Faults greater than 0.231 units
13
Earthquake occurrence by year
14
Earthquake occurrence by depth
15
CONCLUSIONS
  • The lengths of faults follow an exponential
    distribution - this has not been documented and
    may be suggestive of fundamental processes at
    plate boundaries.
  • The spatial occurrence of earthquakes over time
    and with depth is NOT random. This likely
    indicates the current state of stress at the
    plate boundary. There may yet be some hope for
    more complete understanding of tectonics!

16
Future Directions
  • Incorporate bathymetry, gravity and magnetic data
    into map. This has thus far been stymied by the
    format of the ship data.
  • Pursue ideas generated by distribution of fault
    length data. What can the distribution tell us
    about fundamental faulting processes at plate
    boundaries?
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