, was produced by Rawlinson et al. (2015). It includes the Australian Seismological Reference Model (AuSREM) crust, Moho and mantle Kennett and Salmon (2012) in the starting model in order to account for the contribution of unresolved crustal structure in the teleseismic residuals and capture long wavelength features in the mantle that would otherwise be filtered out by the use of a transportable array.