The hot southern continent: heat flow and heat production in Australian Proterozoic terranes
Available 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 of
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|Source:||Geological Society of Australia Special Publication (now Australian Journal of Earth Science)|
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