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Subduction-zone magmatism is triggered by the addition of H(2)O-rich slab-derived components: aqueous fluid, hydrous partial melts, or supercritical fluids from the subducting slab. Geochemical analyses of island arc basalts suggest two slab-derived signatures of a melt and a fluid. These two liquids unite to a supercritical fluid under pressure and temperature conditions beyond a critical endp...

Aalto University, P.O. Box 11000, FI-00076 Aalto www.aalto.fi Author Mikael Mohtaschemi Name of the doctoral dissertation Spatially resolved rheology modeling of complex fluids Publisher School of Science Unit Department of Applied Physics Series Aalto University publication series DOCTORAL DISSERTATIONS 152/2015 Field of research Theoretical and Computational Physics Manuscript submitted 15 Ju...