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Experimental study on the electrical conductivity of quartz andesite at high temperature and high pressure: evidence of grain boundary transport

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Table 1. Whole rock analysis by X-ray fluorescence (XRF) and chemical composition of dominant minerals for quartz andesite by theelectron microprobe (EPMA).
Figure 1. Experimental setup of electrical conductivity measure-ments.
Figure 3. Bode plot of dependence of modulus and phase angleon frequency quartz andesite under conditions of 1.0 GPa and 723–973 K.
Table 2. The value of grain interior, grain boundary and total electri-cal conductivity under 1.0 GPa and 723–973 K
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