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Fig. 8 | Geothermal Energy

Fig. 8

From: The effect of temperature-dependent thermal conductivity on the geothermal structure of the Sydney Basin

Fig. 8

(Volcanics layer is an artificial value adapted from Danis et al. (2012) models, values are listed in Table 2)

Thermal conductivity of sedimentary/coal rocks. Sediment layers are an average value of Triassic Sydney Basin sediments—consisting of coastal samples such as conglomerates, muddy sandstone and medium-grained sandstone. Permian coal layer is an average of the Whittingham, Tomago and Newcastle coal measures

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