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 |
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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 |