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- W2029737516 abstract "[1] Thermal properties of the fault zone materials are of fundamental importance for estimate of frictional heat generation during earthquake. The properties across the Chelungpu fault zone activated by 1999 Chi-Chi earthquake, Taiwan, are measured using the drilled core penetrating the fault zone at around 1100 m depth. The fault zone contains four distinct fracture zones, each of which includes thin slip zones. Thermal conductivity (K) lies between 1.0 and 3.0 Wm−1K−1 and shows the lowest value at the slip zones. Thermal diffusivity (α) varies between 0.8 to 2.0 × 10−6 m2s−1, and is relatively low at the slip zones. Density (ρ) varies between 2200 to 2800 kgm−3 and shows the lowest values at a particular slip zone (1110 m depth). Specific heat (c) is calculated by using above data resulting in the values from 300 to 1000 Jkg−1K−1, and lowest values for slip zones. Using these data and spectral gamma ray logs, reported positive thermal anomalies at the slip zones are re-examined whether they are regarded as residual heat from friction by faulting." @default.
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- W2029737516 date "2007-01-12" @default.
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- W2029737516 title "Thermal properties across the Chelungpu fault zone and evaluations of positive thermal anomaly on the slip zones: Are these residuals of heat from faulting?" @default.
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- W2029737516 doi "https://doi.org/10.1029/2006gl028153" @default.
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