Date post: | 18-Dec-2015 |
Category: |
Documents |
Upload: | caroline-mabel-randall |
View: | 215 times |
Download: | 1 times |
How Shallow Earth Structure Is Determined
A Classroom Exercise Demonstrating Seismic Refraction Use in the Real World
NSTA, St. Louis, 2007John Taber, IRISMichael Wysession, Washington University, St. Louis
Objective(s)
• Explore how refracted seismic waves are used to determine earth structure.
• Reinforce the concepts of reflected and refraction of waves through a real world example.
Time
Distance
Direct wave: Slope is 1/v1
2. Measure Head Wave Slope and you get v2 !!!!
Head wave: Slope is 1/v2
Time
Distance
Direct wave: Slope is 1/v1
3. Measure the cross-over distance, xd , to get the DEPTH to the boundary !!!!
Head wave: Slope is 1/v2
xd
How do you get the depth to the boundary from the cross-over distance, xd ?
Direct wave: TD(x) = x / v1
How do you get the depth to the boundary from the cross-over distance, xd ?
Direct wave: TD(x) = x / v1
Set TD (x) = TH (x)
How do you get the depth to the boundary from the cross-over distance, xd ?
Direct wave: TD(x) = x / v1
Set TD (x) = TH (x)
Depth d
How do you get the depth to the boundary from the cross-over distance, xd ?
Direct wave: TD(x) = x / v1
Set TD (x) = TH (x)
Depth d
3. Measure v1 , v2 , and xd , and you can get the Depth to the boundary!!!!
0 100 km
Mid-Atlantic Ridge off South America
Computer model
Ray trace diagram
What about variable layers?