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Images for off limits; more images...

Images, UC QuakeStudies

Graffiti on a damaged building on Colombo Street. The photographer comments, "This street art has been unseen by the general Christchurch population as it was off limits in the Red Zone".

Audio, Radio New Zealand

Building plans signed off by the Christchurch City Council show one of its own structural engineers was involved in the design of a new multistorey building that is unstable. The eight-storey office building at 230 High Street is off-limits as it is too weak and might 'rupture' in an earthquake. But the council insists the planning documents are wrong and its engineer had only a minor role. Phil Pennington reports.

Images, UC QuakeStudies

The side of the Empire Hotel on London Street in Lyttelton where the brick wall has crumbled. Bracing has been placed on the front of the building to keep it together and limit further damage from aftershocks. The building has been cordoned off with fencing.

Images, UC QuakeStudies

A photograph of the Cranmer Centre on Armagh Street. Bricks have fallen off one of the gables onto the concrete below. The remaining gables have been braced with wood to limit further damage. A cherry picker can be seen below, and there is fencing around the building.

Images, UC QuakeStudies

A view down London Street in Lyttelton. The road has been closed to traffic because of unstable and damaged buildings in the area. In the background is the Empire Hotel on London Street in Lyttelton. Bracing has been placed on the front of the building to keep it together and limit further damage from aftershocks. The building has been cordoned off with fencing.

Images, UC QuakeStudies

A view down London Street in Lyttelton. The road has been closed to traffic because of unstable and damaged buildings in the area. In the background is the Empire Hotel on London Street in Lyttelton. Bracing has been placed on the front of the building to keep it together and limit further damage from aftershocks. The building has been cordoned off with fencing.

Images, UC QuakeStudies

A digitally manipulated image of the Lawrie and Wilson Auctioneers building on Tuam Street. The photographer comments, "This building at 210 Tuam Street is still off limits after the Christchurch earthquake. It has Lawrie and Wilson Auctioneers at the top and Christchurch City Council below. In the past it had a City Photography and at a different time a Parking Unit sign".

Images, UC QuakeStudies

The feet of a fallen mannequin rest against a shop window. The photographer comments, "It is enough to make your toes curl. This is a mannequin that has been on its back since this clothing store was cleared out after the Christchurch earthquake. The store, which is in the earthquake red zone, has been off limits and untouched in the for two years".

Images, UC QuakeStudies

A view down London Street in Lyttelton. The road has been closed to traffic because of unstable and damaged buildings in the area. In the background is the Empire Hotel on London Street in Lyttelton. Bracing has been placed on the front of the building to keep it together and limit further damage from aftershocks. The building has been cordoned off with fencing.

Images, UC QuakeStudies

A digitally manipulated image of a shop window. A vase is visible in the window, and the sillhouette of a mannequin in the background. The photographer comments, "The title came from the pot and the E on the window. This is a building that has been off limits since the Christchurch earthquake. The E was sprayed on the window by rescue teams after searching the building and finding it was empty. This is a very old wooden building that looks OK from the front, but terrible from the side as the previously adjoined building has been demolished.

Images, UC QuakeStudies

The sign for Perry's Cafe has had "Shaken but not deterred" added under the name of the cafe. One of the iconic figures of two workmen painted on the side of the building, which have regularly-changed speech bubbles commenting humorously on topical subjects, are saying "Is my crack showing?" The paint has peeled from the other speech bubble, obscuring the reply. The photographer comments, "After the numerous earthquakes in Christchurch a lot of buildings were damaged and made off limits. This affected a lot of cafes and take aways, so if you were open you needed to make it known. The words missing from the speech bubble are 'Don't be silly'".

Research papers, University of Canterbury Library

This poster presents work to date on ground motion simulation validation and inversion for the Canterbury, New Zealand region. Recent developments have focused on the collection of different earthquake sources and the verification of the SPECFEM3D software package in forward and inverse simulations. SPECFEM3D is an open source software package which simulates seismic wave propagation and performs adjoint tomography based upon the spectral-element method. Figure 2: Fence diagrams of shear wave velocities highlighting the salient features of the (a) 1D Canterbury velocity model, and (b) 3D Canterbury velocity model. Figure 5: Seismic sources and strong motion stations in the South Island of New Zealand, and corresponding ray paths of observed ground motions. Figure 3: Domain used for the 19th October 2010 Mw 4.8 case study event including the location of the seismic source and strong motion stations. By understanding the predictive and inversion capabilities of SPECFEM3D, the current 3D Canterbury Velocity Model can be iteratively improved to better predict the observed ground motions. This is achieved by minimizing the misfit between observed and simulated ground motions using the built-in optimization algorithm. Figure 1 shows the Canterbury Velocity Model domain considered including the locations of small-to-moderate Mw events [3-4.5], strong motion stations, and ray paths of observed ground motions. The area covered by the ray paths essentially indicates the area of the model which will be most affected by the waveform inversion. The seismic sources used in the ground motion simulations are centroid moment tensor solutions obtained from GeoNet. All earthquake ruptures are modelled as point sources with a Gaussian source time function. The minimum Mw limit is enforced to ensure good signal-to-noise ratio and well constrained source parameters. The maximum Mw limit is enforced to ensure the point source approximation is valid and to minimize off-fault nonlinear effects.

Audio, Radio New Zealand

ANDREW LITTLE to the Prime Minister: Does he stand by his statement that “Nick Smith has dealt with some of the most complex problems of resource law and housing more successfully than any other politician here could have”; if so, in what ways, if any, does he think the housing situation for New Zealanders has improved under Hon Nick Smith? BRETT HUDSON to the Minister of Finance: What steps is the Government taking to improve productivity in the public service? MARAMA FOX to the Minister of Health: Does he agree with counsellor Andrew Hopgood, regarding P addicts, that “… a lack of detox and live-in rehabilitation centres limits options for addicts seeking help”; if so, what is he doing to address this shortage? JONATHAN YOUNG to the Minister for Economic Development: What update can he give on ways the Government is supporting economic development in the Gisborne region? CHRIS HIPKINS to the Associate Minister of Education: How many schools across the country are currently using libraries, halls, and other areas not intended for regular teaching as temporary classrooms? ANDREW BAYLY to the Minister of Justice: What recent announcements has she made regarding phase two of the anti-money laundering and counter-financing of terrorism regime? CATHERINE DELAHUNTY to the Minister for the Environment: Will he put a moratorium on bottled water exports, in response to a 15,000 strong petition and nationwide rallies on water issues taking place today? KELVIN DAVIS to the Minister for Māori Development: Does he have confidence that his leadership of Te Puni Kōkiri and its programmes are resulting in the best outcomes for Māori? MAUREEN PUGH to the Minister of Education: What announcements has she made about the Government’s education-related Better Public Services targets? Dr DAVID CLARK to the Minister of Health: How much did the Canterbury District Health Board receive from the Government for mental health and addiction services support in response to the Kaikōura earthquake, after paying off the debt of Kaikōura’s health centre? Rt Hon WINSTON PETERS to the Minister of Foreign Affairs: Does he stand by all his statements; if so, why? Dr PARMJEET PARMAR to the Minister for Disability Issues: What recent announcements has she made regarding a nationwide transformation of the disability support system?

Research papers, University of Canterbury Library

Bulk rock strength is greatly dependent on fracture density, so that reductions in rock strength associated with faulting and fracturing should be reflected by reduced shear coupling and hence S-wave velocity. This study is carried out along the Canterbury rangefront and in Otago. Both lie within the broader plate boundary deformation zone in the South Island of New Zealand. Therefore built structures are often, , located in areas where there are undetected or poorly defined faults with associated rock strength reduction. Where structures are sited near to, or across, such faults or fault-zones, they may sustain both shaking and ground deformation damage during an earthquake. Within this zone, management of seismic hazards needs to be based on accurate identification of the potential fault damage zone including the likely width of off-plane deformation. Lateral S-wave velocity variability provides one method of imaging and locating damage zones and off-plane deformation. This research demonstrates the utility of Multi-Channel Analysis of Surface Waves (MASW) to aid land-use planning in such fault-prone settings. Fundamentally, MASW uses surface wave dispersive characteristics to model a near surface profile of S-wave velocity variability as a proxy for bulk rock strength. The technique can aid fault-zone planning not only by locating and defining the extent of fault-zones, but also by defining within-zone variability that is readily correlated with measurable rock properties applicable to both foundation design and the distribution of surface deformation. The calibration sites presented here have well defined field relationships and known fault-zone exposure close to potential MASW survey sites. They were selected to represent a range of progressively softer lithologies from intact and fractured Torlesse Group basement hard rock (Dalethorpe) through softer Tertiary cover sediments (Boby’s Creek) and Quaternary gravels. This facilitated initial calibration of fracture intensity at a high-velocity-contrast site followed by exploration of the limits of shear zone resolution at lower velocity contrasts. Site models were constructed in AutoCAD in order to demonstrate spatial correlations between S-wave velocity and fault zone features. Site geology was incorporated in the models, along with geomorphology, river profiles, scanline locations and crosshole velocity measurement locations. Spatial data were recorded using a total-station survey. The interpreted MASW survey results are presented as two dimensional snapshot cross-sections of the three dimensional calibration-site models. These show strong correlations between MASW survey velocities and site geology, geomorphology, fluvial profiles and geotechnical parameters and observations. Correlations are particularly pronounced where high velocity contrasts exist, whilst weaker correlations are demonstrated in softer lithologies. Geomorphic correlations suggest that off-plane deformation can be imaged and interpreted in the presence of suitable topographic survey data. A promising new approach to in situ and laboratory soft-rock material and mass characterisation is also presented using a Ramset nail gun. Geotechnical investigations typically involve outcrop and laboratory scale determination of rock mass and material properties such as fracture density and unconfined compressive strength (UCS). This multi-scale approach is espoused by this study, with geotechnical and S-wave velocity data presented at multiple scales, from survey scale sonic velocity measurements, through outcrop scale scanline and crosshole sonic velocity measurements to laboratory scale property determination and sonic velocity measurements. S-wave velocities invariably increased with decreasing scale. These scaling relationships and strategies for dealing with them are investigated and presented. Finally, the MASW technique is applied to a concealed fault on the Taieri Ridge in Macraes Flat, Central Otago. Here, high velocity Otago Schist is faulted against low velocity sheared Tertiary and Quaternary sediments. This site highlights the structural sensitivity of the technique by apparently constraining the location of the principal fault, which had been ambiguous after standard processing of the seismic reflection data. Processing of the Taieri Ridge dataset has further led to the proposal of a novel surface wave imaging technique termed Swept Frequency Imaging (SFI). This inchoate technique apparently images the detailed structure of the fault-zone, and is in agreement with the conventionally-determined fault location and an existing partial trench. Overall, the results are promising and are expected to be supported by further trenching in the near future.