1887

Abstract

We tried to determine the velocity discontinuities in the crust and uppermost mantle using receiver function method. After calculation of receiver functions, we convert the time axis to the depth axis and we observed 2-D images up to 80 km depth. This study showed the Moho depth changes place by place between 25 and 35 km in western Turkey.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.126.6246
2009-05-10
2021-10-24
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.126.6246
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error