Deep fluids in subducted continental crust
Date
2013
Authors
Hermann, Joerg
Zheng, Fei Zheng
Rubatto, Daniela
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Mineralogical Society of America
Abstract
Observations from ultrahigh-pressure metamorphic rocks combined with experimentally determined phase relations provide a framework for understanding fluid-mediated mass transfer in deeply subducted continental crust. At temperatures below 650 °C, aqueous
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Keywords: continental crust; crustal deformation; mass transfer; observational method; P-T conditions; partial melting; phengite; rheology; subduction zone; ultrahigh pressure metamorphism; zircon Fluids; Partial melting; Phengite; Subduction; UHP metamorphism; Zircon
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2037-12-31
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