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morphogenic earthquakes (Quigley et al ., 2010 ; Clark et al ., 2012 ) . Long-term patterns
in large earthquake occurrence, both temporal and spatial, can be deduced from the land-
scape record and used to inform contemporary earthquake hazard science. Seismicity
source parameters such as large earthquake recurrence and magnitude vary across the
Australian continent, and can be interpreted in a framework of large-scale neotectonic
domains defined on the basis of geology and crustal setting (Clark et al ., 2012 ) . Temporal
and spatial clustering of earthquakes is apparent at the scale of a single fault, and at the
1,000 km scale of a domain. The utility of the domains approach, which ties seismicity char-
acteristics to crustal architecture and geology, is that behaviours might be extrapolated from
well-characterised regions to poorly known analogous regions, both within Australia and
worldwide.
Acknowledgements
This paper is published with the permission of the CEO of Geoscience Australia. The
authors would like to thank Marcelo Assump¸ ao and Pradeep Talwani for providing review
comments that improved the manuscript. Mark Leonard and David Burbidge are also
thanked for their constructive reviews.
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