The 2010–2011 Canterbury earthquake sequence: Environmental effects, seismic triggering thresholds and geologic legacy

MC Quigley, MW Hughes, BA Bradley, S van Ballegooy… - Tectonophysics, 2016 - Elsevier
Seismic shaking and tectonic deformation during strong earthquakes can trigger widespread
environmental effects. The severity and extent of a given effect relates to the characteristics …

[HTML][HTML] Paleoliquefaction studies and the evaluation of seismic hazard

MP Tuttle, R Hartleb, L Wolf, PW Mayne - Geosciences, 2019 - mdpi.com
Recent and historical studies of earthquake-induced liquefaction, as well as
paleoliquefaction studies, demonstrate the potential usefulness of liquefaction data in the …

System response of liquefiable deposits

M Cubrinovski, A Rhodes, N Ntritsos… - Soil Dynamics and …, 2019 - Elsevier
Detailed geotechnical characterization and in-depth liquefaction assessment using seismic
effective stress analyses are presented for 55 liquefaction case histories (sites) from …

Near-source strong ground motions observed in the 22 February 2011 Christchurch earthquake

BA Bradley, M Cubrinovski - Seismological Research …, 2011 - pubs.geoscienceworld.org
On 22 February 2011 at 12: 51 pm local time, a moment magnitude Mw 6.3 earthquake
occurred beneath the city of Christchurch, New Zealand, causing an level of damage and …

Soil liquefaction effects in the central business district during the February 2011 Christchurch earthquake

M Cubrinovski, JD Bray, M Taylor… - Seismological …, 2011 - pubs.geoscienceworld.org
During the period between September 2010 and June 2011, the city of Christchurch was
strongly shaken by a series of earthquakes that included the 4 September 2010 (Mw= 7.1) …

The Mw 6.2 Christchurch earthquake of February 2011: preliminary report

A Kaiser, C Holden, J Beavan, D Beetham… - New Zealand journal …, 2012 - Taylor & Francis
Abstract A moment magnitude (Mw) 6.2 earthquake struck beneath the outer suburbs of
Christchurch, New Zealand's second largest city, on 22 February 2011 local time. The …

[HTML][HTML] 8th Ishihara lecture: Holistic evaluation of liquefaction response

M Cubrinovski, N Ntritsos - Soil Dynamics and Earthquake Engineering, 2023 - Elsevier
Soil liquefaction during earthquakes is a highly dynamic process involving rapid
development of excess pore water pressures (EPWP), reduction in soil stiffness and …

The Darfield (Canterbury, New Zealand) Mw 7.1 Earthquake of September 2010: A Preliminary Seismological Report

K Gledhill, J Ristau, M Reyners… - Seismological …, 2011 - pubs.geoscienceworld.org
At 04: 35 on Saturday 4 September 2010 local time (16: 35 on 3 September UT) a moment
magnitude (Mw) 7.1 earthquake struck approximately 10 km southeast of the town of …

Select liquefaction case histories from the 2010–2011 Canterbury earthquake sequence

RA Green, M Cubrinovski, B Cox, C Wood… - Earthquake …, 2014 - journals.sagepub.com
The 2010–2011 Canterbury earthquake sequence began with the 4 September 2010, Mw7.
1 Darfield earthquake and includes up to ten events that induced liquefaction. Most notably …

[HTML][HTML] Influence of non-plastic fines content on maximum shear modulus of granular materials

M Goudarzy, MM Rahman, D König, T Schanz - Soils and Foundations, 2016 - Elsevier
Resonant column tests were conducted on clean Hostun sand and Hostun sand mixed with
5%, 10%, 20%, 30% and 40% fines (particle size smaller than 0.075 mm) to assess the …