Seismic velocity structure of the crust and shallow mantle of the Central and Eastern United States by seismic surface wave imaging
Abstract Seismic surface waves from the Transportable Array of EarthScope's USArray are used to estimate phase velocity structure of 18 to 125 s Rayleigh waves, then inverted to obtain three‐dimensional crust and upper mantle structure of the Central and Eastern United States (CEUS) down to ∼200 km....
שמור ב:
| Principais autores: | , |
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| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
Wiley
2016-01-01
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| סדרה: | Geophysical Research Letters |
| נושאים: | |
| גישה מקוונת: | https://doi.org/10.1002/2015GL066637 |
| תגים: |
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