Abstract
The effects of multiple phase transitions on mantle convection are investigated by numerical simulations that are based on three-dimensional models. These simulations show that cold sheets of mantle material collide at junctions, merge, and form a strong downflow that is stopped temporarily by the transition zone. The accumulated cold material gives rise to a strong gravitational instability that causes the cold mass to sink rapidly into the lower mantle. This process promotes a massive exchange between the lower and upper mantles and triggers a global instability in the adjacent plume system. This mechanism may be cyclic in nature and may be linked to the generation of superplumes.
Original language | English (US) |
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Pages (from-to) | 1308-1311 |
Number of pages | 4 |
Journal | Science |
Volume | 259 |
Issue number | 5099 |
DOIs | |
State | Published - 1993 |