Heat Flow in Southern Australia and Connections With East Antarctica
Alicia Pollett, Derrick Hasterok, Tom Raimondo, JA Halpin, Martin Hand, Betina Bendall, Sandra McLaren
Abstract
Alicia Pollett, Derrick Hasterok, Tom Raimondo, JA Halpin, Martin Hand, Betina Bendall, Sandra McLaren
Abstract
Key Points First heat flow measurements from the Coompana Province, southern Australia, indicate values of 40–70 mW/m2 (57 ± 3 mW/m2 average) A tectonically reconstructed heat flow map constrains the thermal regime of geological provinces formerly contiguous with East Antarctica Geophysical models of Antarctic heat flow are likely underestimating crustal sources of radiogenic heat that influence subglacial melting
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Key Points First heat flow measurements from the Coompana Province, southern Australia, indicate values of 40–70 mW/m2 (57 ± 3 mW/m2 average) A tectonically reconstructed heat flow map constrains the thermal regime of geological provinces formerly contiguous with East Antarctica Geophysical models of Antarctic heat flow are likely underestimating crustal sources of radiogenic heat that influence subglacial melting
Key concepts: Radiogenic nuclide, Heat flow, Geology, Flow (mathematics), High heat, Geophysics, Thermal, Mantle (geology)