Abstract
Numerical models of mantle convection are starting to reproduce many of the essential features of continental drift and plate tectonics. The authors show how such methods can integrate a wide variety of geophysical and geological observations.
| Original language | English |
|---|---|
| Pages (from-to) | 22-33 |
| Number of pages | 12 |
| Journal | Computing in Science and Engineering |
| Volume | 2 |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - 2000 |
| Externally published | Yes |