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Swiss Journal of Geosciences
Fig. 8 | Swiss Journal of Geosciences

Fig. 8

From: The Saint-Ursanne earthquakes of 2000 revisited: evidence for active shallow thrust-faulting in the Jura fold-and-thrust belt

Fig. 8

Vertical-component waveforms of selected earthquakes in the the Saint-Ursanne region recorded at station BOURR. Z is the focal depth in kilometers resulting from the relative relocations shown in Fig. 5. Colors denote origin time. Note the differences in waveform characteristics between near-surface sources (event 1–6, including the sequence of 2000) and sources likely located in the Paleozoic crystalline basement (event 7–11). See text for details

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