The timescale for segregation and transport of basaltic melts, which are ultimately responsible for formation of the Earth's crust, is critically dependent on the permeability of the partly molten asthenospheric mantle, yet this permeability is known mainly from semi-empirical and analogue models. A high-pressure, high-temperature centrifuge is now used to measure the rate of basalt melt flow in olivine aggregates; the resulting permeabilities are one to two orders of magnitude larger than predicted by current parameterizations.
- James A. D. Connolly
- Max W. Schmidt
- Nikolai Bagdassarov