1887

Abstract

In principle, nonlinear inversion that finds the distribution of elastic parameters in the Earth whose synthetic data best matches the observed data is an ideal inversion. All seismic wave phenomena such as reflected waves, mode-conversions, refracted waves, transmitted waves, Rayleigh waves etc. are used to obtain the inversion result.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201410846
1991-05-28
2020-04-08
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410846
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