Processes of melt generation in subduction zones are discussed, based on numerical calculations taking account of the flow pattern, energy balance and phase equilibrium constraints for H
2O-bearing peridotites. A significant amount of melt is newly found to be produced in the downward flow along the plate by compression melting, corresponding to a gentle or negative
dT/dP slope of the solidus curve. The amount of melt produced is comparable to the eruption rate of magmas on volcanic arcs (i.e., 10
0 to 10
2km
3/million year per 1km of the arc length). Although further studies on the distribution of H
2O and melt segregation processes are required for accurate estimates, compression melting in subduction zones is probably inevitable.
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