Abstract
Growing evidence from a variety of geologic indicators points to significant topography maintained convectively by viscous stresses in the mantle. However, while gravity is sensitive to dynamically supported topography, there are only small free-air gravity anomalies (<30mGal) associated with Earth's long-wavelength topography. This has been used to suggest that surface heights computed assuming a complete isostatic equilibrium provide a good approximation to observed topography. Here we show that the apparent paradox is resolved by the well-established formalism of global, self-gravitating, viscously stratified Earth models. The models predict a complex relation between dynamictopography, mass, and gravity anomalies that is not summarized by a constant admittancei.e., ratio of gravity anomalies to surface deflectionsas one would infer from analytic flow solutions formulated in a half-space. Our results suggest that sizable dynamic topography may exist without a corresponding gravity signal.
| Dokumententyp: | Zeitschriftenartikel |
|---|---|
| Fakultät: | Geowissenschaften > Department für Geo- und Umweltwissenschaften |
| Themengebiete: | 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie |
| ISSN: | 0094-8276 |
| Sprache: | Englisch |
| Dokumenten ID: | 48859 |
| Datum der Veröffentlichung auf Open Access LMU: | 27. Apr. 2018 08:16 |
| Letzte Änderungen: | 04. Nov. 2020 13:26 |
