Our knowledge of magma dynamics would be improved if geophysical data could be used to infer rheological constraints in melt-bearing zones. Geophysical images of the Earth's interior provide frozen snapshots of a dynamical system. However, knowledge of a rheological parameter such as viscosity would constrain the time-dependent dynamics of melt bearing zones. We propose a model that relates melt viscosity to electrical conductivity for naturally occurring melt compositions (including H2O) and temperature. Based on laboratory measurements of melt conductivity and viscosity, our model provides a rheological dimension to the interpretation of electromagnetic anomalies caused by melt and partially molten rocks (melt fraction ~ >0.7).
Pommier, A., Evans, R. L., Key, K., Tyburczy, J. A., Mackwell, S., & Elsenbeck, J. (2013). Prediction of silicate melt viscosity from electrical conductivity: A model and its geophysical implications. Geochemistry, Geophysics, Geosystems, 14(6), 1685–1692. doi:10.1002/ggge.20103
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