3D thermal convection simulations of the McArthur River mineral system

Results of simulations of fluid flow and heat transport in a 3D model of the McArthur River (HYC) Zn-Pb-Ag mineral system in the Northern Territory, Australia. The model comprises a simplified representation of the 3D architecture of the Batten Fault Zone in the southern McArthur Basin, comprising a single steeply dipping fault intersecting a gently dipping hydro-stratigraphic sequence.\nThe results are presented as a series of Exodus files (for 3D visualisation) and CSV files (containing the time history of selected variables over the course of each simulation). Exodus files can be viewed using Paraview (https://www.paraview.org).\nLineage: The simulations were performed using the open-source finite element code MOOSE (https://www.mooseframework.org).