McLaren, SandraSandiford, Michael. AHand, MartinNeumann, NWyborn, Lesley ABastrakova, I.2015-12-132015-12-130072-1085http://hdl.handle.net/1885/87996Available surface heat-flow measurements from Australian Proterozoic terranes (83 ± 18 mWm-2) are significantly higher than the global Proterozoic average of -50 mWm-2. Seismic evidence for the presence of relatively cool mantle together with the lack ofKeywords: Continental crust; Heat budget; Heat flow; Proterozoic; Terranes200310.1130/0-8137-2372-8.1572016-02-24