Fluids and melts liberated from subducting oceanic crust recycle lithophile elements back into the mantle wedge, facilitate melting, and ultimately lead to prolific subduction-zone arc volcanism.
- precision note: This supersedes the Phase 2 hypothesis that water lowers the melting temperature of rock. The retrieved Tier A source states that liberated fluids facilitate melting; it does not state a melting-point depression as a general property of water in rock, and Lithoen therefore asserts the narrower statement the source supports.
- method: Experimental petrology with direct laser-ablation ICP-MS analysis of fluids and melts equilibrated with basaltic eclogite.
Evidence support: Supported by the cited evidence one source
Evidence: Kessel 2005 Peer-reviewed