Three-Dimensional Seismic Ray Tracing in a Laterally Heterogeneous Spherical Earth
Abstract
It is the purpose of this study to present a basic, computer-oriented method of tracing seismic rays, either for P or S waves, propagating through a laterally heterogeneous spherical earth. This method is especially designed to consider a class of lateral seismic heterogeneities related to sea-floor spreading and global tectonics, e.g., the deep structure beneath mid-oceanic ridges and island arcs, the sources and sinks, respectively, in a system of drifting lithospheric plates.
Document Details
- Document Type
- Technical Report
- Publication Date
- May 20, 1970
- Accession Number
- AD0719970
Entities
People
- Klaus H. Jacob
Organizations
- Lamont–Doherty Earth Observatory