Fig. 15From: The 1905 Chamonix earthquakes: active tectonics in the Mont Blanc and Aiguilles Rouges massifsFits 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 Back to article page