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Fig. 15 | Swiss Journal of Geosciences

Fig. 15

From: The 1905 Chamonix earthquakes: active tectonics in the Mont Blanc and Aiguilles Rouges massifs

Fig. 15

Fits of the Göttingen (GTT) and Uppsala (UPP) filtered Wiechert records for the focal mechanism of the Remuaz fault and a focal depth of 5 km (F2 in Table 3). Recorded traces (in black) and computed traces (in red) are normalized. Yellow zones indicate the time intervals where computation of correlation r and misfit m are calculated. The ∆ on the left is the epicentral distance, A is the amplitude of the filtered signals (band-pass between 0.02 and 0.07 Hz in GTT, 0.02 and 0.05 Hz in UPP), w is the weight applied to each trace in the computation of r and m. Note that because of the filtering process, amplitudes A are smaller than those of the original records shown in Figs. 12 and 13

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