Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8143719 | Planetary and Space Science | 2014 | 44 Pages |
Abstract
Simulations that neglect the time-dependence of internal heat sources on the other hand tend to lead to an increasing likelihood of plate tectonics with increasing mass. Finally, our investigations suggest that a wet rheology does not necessarily favor plate tectonics, but - depending on the reference viscosity - may rather lead to a stagnant-lid regime.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geophysics
Authors
Lena Noack, Doris Breuer,