Geochemistry of continental subduction-zone fluids
The composition of continental subduction-zone fluids varies dramatically from dilute aqueous solutions at subsolidus conditions to hydrous silicate melts at supersolidus conditions, with variable concentrations of fluid-mobile incompatible trace elements. At ultrahigh-pressure (UHP) metamorphic conditions, supercritical fluids may occur with variable compositions. The water component of these fluids primarily derives from structural hydroxyl and molecular water in hydrous and nominally...[Show more]
|Collections||ANU Research Publications|
|Source:||Earth, Planets and Space|
|01_Zheng_Geochemistry_of_continental_2014.pdf||2.37 MB||Adobe PDF|
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