Table 3 Five focal mechanisms Fn (strike ϕ, dip δ, rake λ), three depths h, and half duration τ/2 are used for computing the seismic waveforms at Göttingen and Uppsala (see also Fig. 6)
From: The 1905 Chamonix earthquakes: active tectonics in the Mont Blanc and Aiguilles Rouges massifs
