“…For instance, many interpretations conclude by requiring that Tasmania shifts some hundreds of km along an eastwest, either sinistral or dextral Palaeozoic strike-slip fault in Bass Strait (Harrington et al, 1973;Baillie, 1985;Stump et al, 1986;Elliott and Gray, 1992;Betts et al, 2002), often referred to as the Colac-Rosedale Fault. However, there is a lack of evidence for the existence of this fault from available data (e.g., modern magnetic and gravity datasets do not show evidence for any lateral offset between Tasmania and Victoria), including no persuasive along-strike correlation in terms of stratigraphy and metamorphic history.…”