| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4695302 | Tectonophysics | 2006 | 20 Pages |
Abstract
Scattered arrivals, which trail the reflection from the '410' discontinuity and a reflection from a shallower depth of â¼320 km, constrain heterogeneity around the top of the transition zone. This heterogeneity is modelled by fluctuations in the 320-460 km depth interval with correlation lengths on the order of 20-40 km by 5-10 km. Scattering from the two shallower heterogeneous zones improves the description of the phases from around the transition zone.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
L. Nielsen, H. Thybo,