| Autor: |
Filmer, P. E., McNutt, M. K. |
| Zdroj: |
Marine Geophysical Researches; June 1989, Vol. 11 Issue: 2 p77-87, 11p |
| Abstrakt: |
The Canary Islands geoid anomaly shows only a short-wavelength high associated with island topography. The predicted anomaly best matches the observed geoid when we assume that the lithosphere is a very stiff plate. We find no evidence for shallow reheating or a mantle plume, since there is no evidence of a midplate swell and the corresponding elastic thickness is appropriate for the age of the seafloor on which the island group rests. |
| Databáze: |
Supplemental Index |
| Externí odkaz: |
|
Full text from SpringerLink