Fig. 2From: The effect of temperature-dependent thermal conductivity on the geothermal structure of the Sydney BasinCalibration thermal conductivity for a—stainless steel sample (19.05 mm) high error margin at 20 °C for stainless steel sample, b—vespel 1 (3.175 mm) high error margin at 20 °C for vespel 1, c—vespel 2 (9.525 mm) high error margin at 20 °C for vespel 2. Error margin persistently decreases at higher temperaturesBack to article page