Abstract
Summary The terrestrial heat flux was determined at two sites in Tasmania. At Glenorchy (147° 15′ E, 42° 50′ S) it was 87 mWm−2 in a dolerite section centred at 350 m depth. At Olga Ridge (145° 47′ E, 42° 46′ S) it was 57 mWm−2 in a mudstone section centred at 250 m.
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