Optimal equations of state for mantle minerals from simultaneous non-linear inversion of multiple datasets
A fully non-linear inversion scheme is introduced for the determination of the parameters controlling the equation of state of mineral phases using the thermodynamically consistent formulation introduced recently by Stixrude and Lithgow-Bertelloni. The formulation is based on a directed search in an eight-dimensional parameter space using the neighbourhood algorithm developed by Sambridge to search for the minimum of an objective function derived from the misfit to multiple data sets that...[Show more]
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|Source:||Physics of the Earth and Planetary Interiors|
|01_Kennett_Optimal_equations_of_state_for_2009.pdf||1.5 MB||Adobe PDF||Request a copy|
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