The objective of this example is to examine the effect of shallow low velocity sediments on the receiver function. A halfspace and a simple crustal model are considered.
Download the package RFTN3.tgz. Then do the following:
gunzip -c RFTN3.tgz | tar xvf - cd RFTN3 ./DOIT
The script will create the figures shown below. The script requires CPS programs hrftn96, gsac and plotnps and the ImageMagick package program convert to transform the EPS files to a PNG image.
![]() Halfspace model for ALP=1.0 |
![]() Halfspace model for ALP=2.5 |
![]() Halfspace model for ALP=5.0 |
![]() Crustal model for ALP=1.0 |
![]() Crustal model for ALP=2.5 |
![]() Crustal model for ALP=5.0 |
![]() Overlay of halfspace (red) and crustal (blue) base models for ALP=1.0 |
![]() Overlay of halfspace (red) and crustal (blue) base models for ALP=2.5 |
![]() Overlay of halfspace (red) and crustal (blue) base models for ALP=5.0 |