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Showing 1 to 1 of 1 for “"Gesteinsphysik"”.
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The thermal regime of the Eastern Alps along the TRANSALP profile
The results of petrophysical laboratory measurements and inverse modelling were utilized to estimate the 2-D, steady-state conductive thermal regime in the Eastern Alpine crust and heat flow at the Moho along the TRANSALP profile. Temperature dependence of thermal conductivity and specific heat …