Reverse-time migration-based reflection tomography using teleseismic free surface multiples
Converted and multiply reflected phases from teleseismic events are routinely used to create structural images of the crust–mantle boundary (Moho) and the elasticity contrasts within the crust and upper mantle. The accuracy of these images is to a large extent determined by the background velocity m...
| Principais autores: | , , , |
|---|---|
| Outros Autores: | |
| Formato: | Artigo |
| Idioma: | en_US |
| Publicado em: |
Oxford University Press on behalf of The Royal Astronomical Society
2014
|
| Acesso em linha: | http://hdl.handle.net/1721.1/90857 https://orcid.org/0000-0003-1650-6818 |