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Melting-induced crustal production helps plate tectonics on Earth-like planets
| Content Provider | Semantic Scholar |
|---|---|
| Author | Lourenço, Diogo L. Rozel, A. Tackley, Paul J. |
| Copyright Year | 2016 |
| Abstract | Abstract Within our Solar System, Earth is the only planet to be in a mobile-lid regime. It is generally accepted that the other terrestrial planets are currently in a stagnant-lid regime, with the possible exception of Venus that may be in an episodic-lid regime. In this study, we use numerical simulations to address the question of whether melting-induced crustal production changes the critical yield stress needed to obtain mobile-lid behaviour (plate tectonics). Our results show that melting-induced crustal production strongly influences plate tectonics on Earth-like planets by strongly enhancing the mobility of the lid, replacing a stagnant lid with an episodic lid, or greatly extending the time in which a smoothly evolving mobile lid is present in a planet. Finally, we show that our results are consistent with analytically predicted critical yield stress obtained with boundary layer theory, whether melting-induced crustal production is considered or not. |
| Starting Page | 18 |
| Ending Page | 28 |
| Page Count | 11 |
| File Format | PDF HTM / HTML |
| DOI | 10.1016/j.epsl.2016.01.024 |
| Volume Number | 439 |
| Alternate Webpage(s) | http://jupiter.ethz.ch/~arozel/papers/LourencoRozelTackley2016EPSL.pdf |
| Alternate Webpage(s) | http://www.geo.uu.nl/iGEO/papers/1-s2.0-S0012821X16000467-main.pdf |
| Alternate Webpage(s) | http://www.meetingorganizer.copernicus.org/EGU2016/EGU2016-7770.pdf |
| Alternate Webpage(s) | https://doi.org/10.1016/j.epsl.2016.01.024 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |