Slab pull does takes place at a convergent boundary and subduction zone. Slab pull therefore occurs because subducting slabs are cooler, and therefore more dense, than surrounding asthenosphere.
Subduction often takes place as a result of two plates colliding at a convergent boundary, and one plate is pushed beneath the other, back into the Earth's interior.
A oceanic plate hitting with a continental plate, will cause the denser oceanic plate to push or bent downward and slides under the edge of the continent.
Conclusively, the sinking of the tectonic plate makes the heat from beneath the Earth to melt.
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