Ground motion simulations of great earthquakes on the Alpine Fault: effect of hypocentre location and comparison with empirical modelling

Author:

Bradley Brendon A.123,Bae Sung E.2,Polak Viktor2,Lee Robin L.1,Thomson Ethan M.1,Tarbali Karim1

Affiliation:

1. Department of Civil and Natural Resources Engineering, University of Canterbury, Christchurch, New Zealand

2. QuakeCoRE, University of Canterbury, Christchurch, New Zealand

3. Department of Civil and Environmental Engineering, Stanford University, CA, USA

Publisher

Informa UK Limited

Subject

Earth and Planetary Sciences (miscellaneous),Geology,Geophysics

Reference42 articles.

1. Bae S, Polak V, Clare R, Bradley BA, Razafindrakoto HNT. 2016. QuakeCoRE ground motion simulation computational workflow. Paper presented at: QuakeCoRE Annual Meeting, Wairakei, New Zealand.

2. A 2300-Year Paleoearthquake Record of the Southern Alpine Fault and Fiordland Subduction Zone, New Zealand, Based on Stacked Turbidites

3. Major Earthquakes Occur Regularly on an Isolated Plate Boundary Fault

4. Late Holocene Rupture History of the Alpine Fault in South Westland, New Zealand

5. Bradley BA. 2012. Ground motion comparison of the 2011 Tohoku, Japan and 2010-2011 Canterbury earthquakes: implications for large events in New Zealand. In: New Zealand Society of Earthquake Engineering Annual Conference, Christchurch, New Zealand; p. 8.

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