1 / 12

How DO they actually locate earthquakes?

How DO they actually locate earthquakes?. Alternatives to S-P Triangulation Hubenthal, M. Taber, M. An Inverse Problem. W e know the end product; arrival times W e have a velocity model for Earth and we want to calculate the original event Location Origin time.

trent
Download Presentation

How DO they actually locate earthquakes?

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. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. How DO they actually locate earthquakes? Alternatives to S-P Triangulation Hubenthal, M. Taber, M.

  2. An Inverse Problem • We know the end product; arrival times • We have a velocity model for Earth and • we want to calculate the original event • Location • Origin time Forward Problem = Model parameters → Data Inverse Problem = Data → Model parameters

  3. The bisector method • P arrivals are much easier to pick  • Assumes an extremely simple velocity model 3 1 5 2 6 4 Which station of this record section was closest?

  4. Bisector Steps • Mark and measure path between TATO/WAKE • Find midpoint of path • Draw bisector perpendicular to path • Label Bisector with station names • Determine which side of the bisector was close to the event. • Repeat with TATO/YAK • Repeat with WAKE/YAK • Repeat with additional stations of your choice

  5. Bisector TATO WAKE X Path

  6. Bisector Steps • Mark and measure path between TATO/WAKE • Find midpoint of path • Draw bisector perpendicular to path • Label Bisector with station names • Determine which side of the bisector was close to the event. • Repeat with TATO/YAK • Repeat with WAKE/YAK • Repeat with additional stations of your choice

  7. Solution

  8. Compare to regional seismicity

  9. Earth is Complex PREM Model

  10. Earth is Complex PREM Model

  11. Solution to complexity • Iterative approach  • Solution through the model provides result • Result is run back through the model to see if it matches the observations (forward problem) • Differences used to refine the model to compute a new solution.   • Process continues until some condition is met

  12. In reality • More data • More complex models • Iterative approach

More Related