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Mantle Convection Modeling with Viscoelastic/Brittle Lithosphere: Numerical Methodology and Plate Tectonic Modeling
| Content Provider | Semantic Scholar |
|---|---|
| Author | Moresi, Louis Dufour, Frédéric |
| Copyright Year | 2002 |
| Abstract | Abstract—The earth's tectonic plates are strong, viscoelastic shells which make up the outermost part of a thermally convecting, predominantly viscous layer. Brittle failure of the lithosphere occurs when stresses are high. In order to build a realistic simulation of the planet's evolution, the complete viscoelastic/brittle convection system needs to be considered. A particle-in-cell finite element method is demonstrated which can simulate very large deformation viscoelasticity with a strain-dependent yield stress. This is applied to a plate-deformation problem. Numerical accuracy is demonstrated relative to analytic benchmarks, and the characteristics of the method are discussed. |
| Starting Page | 2335 |
| Ending Page | 2356 |
| Page Count | 22 |
| File Format | PDF HTM / HTML |
| DOI | 10.1007/s00024-002-8738-3 |
| Volume Number | 159 |
| Alternate Webpage(s) | https://hal.archives-ouvertes.fr/hal-00333884/document |
| Alternate Webpage(s) | http://www.tokyo.rist.or.jp/ACES_WS2/extended_abstract/PDF/LouisMoresi.pdf |
| Alternate Webpage(s) | http://hal.archives-ouvertes.fr/docs/00/33/38/84/PDF/Moresi-etal-Pageoph-revised.pdf |
| Alternate Webpage(s) | https://doi.org/10.1007/s00024-002-8738-3 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |