Reaction-induced grain boundary cracking and anisotropic fluid flow during prograde devolatilization reactions within subduction zones
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DOI: 10.1007/s00410-017-1393-6
Abstract: Devolatilization reactions during prograde metamorphism are a key control on the fluid distribution within subduction zones. Garnets in Mn-rich quartz schist within the Sanbagawa metamorphic belt of Japan are characterized by skeletal structures containing abundant… read more here.
Keywords: grain boundary; devolatilization reactions; fluid; fluid flow ... See more keywords