Magmatic arc structure around Mount Rainier, WA, from the joint inversion of receiver functions and surface wave dispersion
The deep magmatic processes in volcanic arcs are often poorly understood. We analyze the shear wave velocity (VS) distribution in the crust and uppermost mantle below Mount Rainier, in the Cascades arc, resolving the main velocity contrasts based on converted phases within P coda via source normaliz...
| Hoofdauteurs: | , , |
|---|---|
| Andere auteurs: | |
| Formaat: | Journal Article |
| Taal: | English |
| Gepubliceerd in: |
2015
|
| Onderwerpen: | |
| Online toegang: | https://hdl.handle.net/10356/106799 http://hdl.handle.net/10220/25173 |