Abstract
It has remained unclear how much of the negative buoyancy force of the slab (FB) is used to pull the trailing plate at the surface into the mantle. Here I present three-dimensional laboratory experiments to quantify the net slab pull force (FNSP) with respect to FB during subduction. Results show that FNSP increases with increasing slab length and dip up to ∼8-12% of FB, making FNSP up to twice as large as the ridge push force. The remainder of FB is primarily used to drive rollback-induced mantle flow (∼70%), to bend the subducting plate at the trench (∼15-30%) and to overcome shear resistance between slab and mantle (0-8%).
| Original language | English |
|---|---|
| Pages (from-to) | L07611 1-5 |
| Journal | Geophysical Research Letters |
| Volume | 31 |
| Issue number | 7 |
| DOIs | |
| Publication status | Published - 16 Apr 2004 |
| Externally published | Yes |