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Landslides in the Sydney Basin - Geoscience Australia

Landslides in the Sydney Basin - Geoscience Australia

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Seismic Hazard <strong>in</strong> <strong>Sydney</strong>Proceed<strong>in</strong>gs of <strong>the</strong> one day workshop<strong>in</strong>strumentation used had limited dynamic range so would go full-scale for even moderate magnitudeearthquakes, so shear wave arrivals could not be read, and <strong>the</strong>se events could not be locatedprecisely. The <strong>in</strong>strumentation had very limited seismic wave frequency bandwidth, limit<strong>in</strong>g tim<strong>in</strong>gprecision and mak<strong>in</strong>g earthquake magnitude estimates very difficult.Figure 2: <strong>Sydney</strong> region earthquakes, 1993 to 2005.S<strong>in</strong>ce 1992, most events larger than magnitude ML 1.5 can be located to a precision of a fewkilometres or better, <strong>in</strong>clud<strong>in</strong>g depth. The dist<strong>in</strong>ctive seismic character of shallow events(earthquakes, blasts and coal m<strong>in</strong>e collapses) with<strong>in</strong> <strong>the</strong> Mesozoic sediments of <strong>the</strong> <strong>Sydney</strong> Bas<strong>in</strong>51

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