Preconditioned iterative methods for Stokes flow problems arising in computational geodynamics

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Numerical modelling of magma dynamics coupled to tectonic deformation of lithosphere and crust (2013, methodology): “However, we prefer to separate this useful step of additional analysis from the simulation of the actual physics, as it renders it more straightforward to relate input or output parameter values to physical quantities of interest (May & Moresi 2008).”
Fluidity: A fully unstructured anisotropic adaptive mesh computational modeling framework for geodynamics (2011, methodology): “Due to the slow convergence of stationary iterative methods, we consider preconditioned Krylov subspace methods only [e.g., Elman et al., 2005; May and Moresi, 2008; Geenen et al., 2009].”
On iterative methods for the incompressible Stokes problem (2011, unknown): “in combination with an approximation of the Schur complement [15, 18, 19].”