Landslides in the Sydney Basin - Geoscience Australia
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 workshopet al. 1979). Elsewhere <strong>in</strong> <strong>the</strong> <strong>Sydney</strong> Bas<strong>in</strong>, for example, to <strong>the</strong> north of Wollongong, <strong>the</strong> highmodern-day stress regime has reactivated pre-exist<strong>in</strong>g fracture systems (Memarian & Fergusson2003).Figure 1 <strong>Sydney</strong> Bas<strong>in</strong> and major structures <strong>in</strong> <strong>the</strong> adjo<strong>in</strong><strong>in</strong>g Lachlan Fold Belt (afterScheibner 1997). Lapstone Structural Complex is marked along with locations of Figures 2and 3. Faults <strong>in</strong> Lachlan Fold Belt: CSF = fault on western marg<strong>in</strong> of Cockbundoon Syncl<strong>in</strong>e,LGF = Lake George Fault, QF = Queanbeyan Fault, MF = Mulwaree Fault, YF = YarralawFault, WFZ = Wiagdon Fault Zone.14