Towards scaling laws for subduction initiation on terrestrial planets: constraints from two-dimensional steady-state convection simulations
The strongly temperature-dependent viscosity of rocks leads to the formation of nearly rigid lithospheric plates. Previous studies showed that a very low yield stress might be necessary to weaken and mobilize the plates, for example, due to water. However, the magnitude of the yield stress remains p...
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Veröffentlicht in: | Progress in earth and planetary science 2015-07, Vol.2 (1), p.1, Article 18 |
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