The aim of this poster is to examine the seismic response of two structural systems when subjected to observed and simulated ground motions (GMs) for the 22 February 2011 (22Feb2011) Christchurch earthquake (Razafindrakoto et al. (2018)) via an automated workflow. The layout and technical details of the automated workflow are described at Motha et. al. (2019).
This paper presents a seismic velocity model of Canterbury, New Zealand based on 3D geologic surfaces and velocities from a range of data sources. The model provides the 3D crustal structure in the region at multiple length scales for seismic wave propagation simulations, such as broadband ground motion and shallow site response analyses related to understanding the ground motions and site responses during the 2010- 2011 Canterbury earthquakes. Pre-Quaternary geologic horizons are calculated based on the reinterpretation of a comprehensive network of seismic reflection surveys from seven different campaigns over the past 50 years, as well as point constraints across an array of petroleum industry drill holes. Particular attention is given to a detailed representation of Quaternary stratigraphy, representing shallow (z<250m) near-surface layers in the model. Seismic velocities are obtained from seismic reflection processing (for Vp) and also recently performed active and passive surface wave analyses (for Vs). Over 1,700 water wells in the region are used to constrain the complex inter-bedded Quaternary stratigraphy (gravels, sands, silts, organics etc.) near the coastline, including beneath urban Christchurch, which has resulted from fluvial deposition and marine regression and transgression. For the near-surface Springston and Christchurch Formations in the Christchurch urban area (z<50m), high-spatial resolution seismic velocities (including Vs30 ) were obtained from over 13,000 cone penetration tests combined with a recently developed CPT-Vs correlation.
This paper presents an examination of ground motion observations from 20 near-source strong motion stations during the most significant 10 events in the 2010-2011 Canterbury earthquake to examine region-specific systematic effects based on relaxing the conventional ergodic assumption. On the basis of similar site-to-site residuals, surfical geology, and geographical proximity, 15 of the 20 stations are grouped into four sub-regions: the Central Business District; and Western, Eastern, and Northern suburbs. Mean site-to-site residuals for these sub-regions then allows for the possibility of non-ergodic ground motion prediction over these sub-regions of Canterbury, rather than only at strong motion station locations. The ratio of the total non-ergodic vs. ergodic standard deviation is found to be, on average, consistent with previous studies, however it is emphasized that on a site-by-site basis the non-ergodic standard deviation can easily vary by ±20%.
An entry from Jennifer Middendorf's blog for 8 February 2013 entitled, "Vote for me!".
An entry from Ruth Gardner's Blog for 01 November 2013 entitled, "Bonus Boost for Blog".
A story submitted by Brenda Greene to the QuakeStories website.
The "Lyttelton Review" newsletter for 8 October 2012, produced by the Lyttelton Harbour Information Centre.
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A story submitted by Joanna Orwin to the QuakeStories website.
Transcript of Bud Chapman's earthquake story, captured by the UC QuakeBox project.
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A video recording of a lecture presented by Professor Jarg Pettinga and Dr Mark Quigley as part of the 2011 University of Canterbury Earthquake Lecture Series.
Transcript of Harry Kitkevics's earthquake story, captured by the UC QuakeBox project.
Transcript of Owen Macintyre's earthquake story, captured by the UC QuakeBox project.
The "Lyttelton Harbour Review" newsletter for 28 January 2013, produced by the Lyttelton Harbour Information Centre.
A copy of the CanCERN online newsletter published on 11 May 2012
This study investigates the uncertainty of simulated earthquake ground motions for smallmagnitude events (Mw 3.5 – 5) in Canterbury, New Zealand. 148 events were simulated with specified uncertainties in: event magnitude, hypocentre location, focal mechanism, high frequency rupture velocity, Brune stress parameter, the site 30-m time-averaged shear wave velocity (Vs30), anelastic attenuation (Q) and high frequency path duration. In order to capture these uncertainties, 25 realisations for each event were generated using the Graves and Pitarka (2015) hybrid broadband simulation approach. Monte-Carlo realisations were drawn from distributions for each uncertainty, to generate a suite of simulation realisations for each event and site. The fit of the multiple simulation realisations to observations were assessed using linear mixed effects regression to generate the systematic source, path and site effects components across all ground motion intensity measure residuals. Findings show that additional uncertainties are required in each of the three source, path, and site components, however the level of output uncertainty is promising considering the input uncertainties included.
Summary of oral history interview with Lianne Dalziel about her experiences of the Canterbury earthquakes.
A copy of the CanCERN online newsletter published on 2 November 2012
Text reads 'One of the many faces of Mother Nature' and the cartoon shows a moon with a seismic graph across it that has taken on the shape of a face. A second version does not have the moon and a third version has the face say 'I have a few faults'. Context - The Christchurch earthquakes.
Three versions of this cartoon are available
Quantity: 3 digital cartoon(s).
Transcript of Laurie Hill's earthquake story, captured by the UC QuakeBox project.
Transcript of Sherrilee's earthquake story, captured by the UC QuakeBox project.
The "Lyttelton Harbour Review" newsletter for 5 August 2013, produced by the Lyttelton Harbour Information Centre.
The "Lyttelton Harbour Review" newsletter for 17 February 2013, produced by the Lyttelton Harbour Information Centre.
An entry from Ruth Gardner's blog for 1 March 2011 entitled, "Day 8, 6pm - inside the Christchurch cordon".
The "Lyttelton Review" newsletter for 29 October 2012, produced by the Lyttelton Harbour Information Centre.
This manuscript provides a critical examination of the ground motions recorded in the near-source region resulting from the 22 February 2011 Christchurch earthquake. Particular attention is given to reconciling the observed spatial distribution of ground motions in terms of physical phenomena related to source, path and site effects. The large number of near-source observed strong ground motions show clear evidence of: forward-directivity, basin generated surface waves, liquefaction and other significant nonlinear site response. The pseudo-acceleration response spectra (SA) amplitudes and significant duration of strong motions agree well with empirical prediction models, except at long vibration periods where the influence of basin-generated surface waves and nonlinear site response are significant and not adequately accounted for in empirical SA models. Pseudo-acceleration response spectra are also compared with those observed in the 4 September 2010 Darfield earthquake and routine design response spectra used in order to emphasise the amplitude of ground shaking and elucidate the importance of local geotechnical characteristics on surface ground motions. The characteristics of the observed vertical component accelerations are shown to be strongly dependent on source-to-site distance and are comparable with those from the 4 September 2010 Darfield earthquake, implying the large amplitudes observed are simply a result of many observations at close distances rather than a peculiar source effect.
Summary of oral history interview with Susan Allen about her experiences of the Canterbury earthquakes.