“…(Powell and Baillie, 1992;Powell et al, 1993;Seymour, 2011). These rocks are part of a larger succession of turbiditic sandstones and mudstones, the Mathinna Supergroup, which forms the pre-Carboniferous basement of the ETT from the Furneaux Islands to Eaglehawk Neck in southeastern Tasmania (Powell et al, 1993). During the Devonian, prior to and following the Tabberabberan Orogeny, large areas of NE Tasmania were subjected to granitoid intrusions (Black et al, 2005).…”