Abstract
The strong and nonlinear fluxing of the transport properties of silicic melts by water is one of the bestknown features of the physical chemistry of silicate melts applied to geochemistry. The decrease in melt viscosity and relaxation time and increase in electrical conductivity and diffusivities have enormous consequences for all stages of the magmatic cycle including segregation and transport of melts, the kinetics of element partitioning between dissolving or growing minerals and their host melts and the efficiency of melt degassing in shallow subvolcanic
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
