Compaction experiments on aggregates of olivine, chromite, and plagioclase in a high-T and high-P centrifuge, on the other hand, have been published over the past decade (Krättli & Schmidt, 2021, Manoochehri & Schmidt, 2014, Schmidt et al. , 2012) and recently summarized in Connolly and Schmidt (2022). These experiments were performed over a range of gravitational accelerations and can be used to constrain the matrix viscosity of these aggregates at intermediate melt fractions.