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6 results for “Kaikoura New Zealand”
New Zealand Wide model 2.3 Qs and Qp models for New Zealand, updated for Kaikoura
<p><em><strong><span>19-Sept-2024</span></strong><span> Full uncompressed versions of the </span><span>New Zealand Wide 2.3 velocity, Qs and Qp model Tables can be obtained from zenodo.org/records/13799996</span><br></em></p> <p><em><strong>21-May-2022</strong> There are updated Vp and Vp/Vs models 2.3, which incorporate the results from the Southern South Island region, at zenodo.org/record/6568301 </em></p> <p>The Qs and Qp New Zealand Wide models 2.3 incorporate the results from the Kaikoura region using aftershocks, published in Geophysical Journal International (Eberhart-Phillips, et al. 2021).</p> <p>The results from that study have been interpolated and merged into the previous New Zealand Wide model 2.2 (zenodo.org/record/3779523).</p> <p> </p> <p>The models are provided in tables, where the Spread Function (SF) shows the resolution, such that where SF<4, there is little information.</p> <p>Qpnzw2p3xyzltln.tbl.txt</p> <p>Qsnzw2p3xyzltln.tbl.txt</p> <p> </p> <p>There are also simul format Q files.</p> <p>Qpnzw2p3.mod.txt</p> <p>Qsnzw2p3.mod.txt</p> <p> </p> <p>Map plots of the Q models, resolution and data</p> <p>KaikouraQ_figures.pdf</p> <p> </p> <p>Q at any point within the 3D gridded models is defined by linearly interpolating between nodes.</p> <p>The models use Transverse Mercator coordinate transformation with a central meridian= 173, and counterclockwise rotation of 140. Earth-flattening transformation is used for velocity during ray-tracing. The depths are relative to sea-level.</p> <p> </p> <p>Reference: Eberhart-Phillips, D., S. Ellis, F. Lanza, and S. Bannister (2021), Heterogeneous material properties – as inferred from seismic attenuation - influenced multiple fault rupture and ductile creep of the Kaikoura Mw 7.8 earthquake, New Zealand, <em>Geophys. J. Int.</em>, doi:10.1093/gji/ggab272. </p>
Landslides from Space - Kaikoura Earthquake-triggered Landslides, New Zealand (14th November 2016)
<p>On 14th November 2016 an earthquake with a maginitude of 7.8 triggered multiple landslides. Especially the village of Kaikoura was affected as it was cut off from the rest of New Zealand when its main road, State Highway 1. was blocked through multiple rockfalls and landslides.<br> <br> The pre-event acquisition is from 14th September 2016 (Sentinel-2) and the post-event acquisition is from 15th December 2016 (Sentinel-2).<br> <br> <em>Contains modified Copernicus Sentinel data (2016)</em></p>
Map of Co-Seismic Landslides for the M 7.8 Kaikoura, New Zealand Earthquake
<p>Prepared by the Research Group on Earthquake Geology in Greece (http://eqgeogr.weebly.com/)</p> <p>Version 2 (updated)</p> <p>With the release of new Sentinel-2 images, and other available resources for the M7.8 Kaikoura earthquake, we present an update of the Map of Co-Seismic Landslides and Surfaces Ruptures (As of 27/11/2016). Landslides were mapped using Sentinel-2 satellite images from Copernicus, European Space Agency, dated November and December 2016. Images were visually compared with previous last available S2A images without cloud cover (13 September and 26 October) and landslides and large slope failures were manually mapped. Areas covered by cloud are omitted and shown on map. 5875 landslide sites are shown in the map. A small number of landslides could have been mis-identified due to insufficient resolution of the images, small gaps of cloud cover or for other reasons. Also, re-activated landslides on the central mountainous area were unabled to identify due to imagery restrictions (medium resolution, relief shadows etc). Some local gaps in Sentinel imagery still exist due to cloud cover, but we believe the current map is very close to the major distribution of mass movement effects. Surface ruptures were mapped using Sentinel-2 imagery and approximate position from photos of the post-earthquake aerial surveys of Environment Canterbury Regional Council (http://ecan.govt.nz)</p> <p>KML file contains7355 landslide spots.</p>
Foraminiferal insights into the complexities of the turbidity currents triggered by the 2016 Kaikoura Earthquake, New Zealand, Supplementary Appendices
<p>This data set and cluster analysis dendrogram support the published article.</p> <p>Supplementary Appendix 1. Measured foraminiferal data for 2016 Kaikōura turbidite and pre-turbidite samples. </p> <p>Supplementary Appendix 2. Cluster analysis dendrogram of foraminiferal samples based on the relative abundance of tests >125 µm of the key benthic “genera” (Table 2) using Bray Curtis similarity coefficient.</p>
Fault geometry of the 2016 Mw 7.8 Kaikoura earthquake, New Zealand
<p>Citation:</p> <p>Xu, W., Feng, G., Meng, L., Zhang, A., Ampuero, J. P., Bürgmann, R., & Fang, L. (2018). Transpressional rupture cascade of the 2016 Mw 7.8 Kaikoura earthquake, New Zealand. Journal of Geophysical Research: Solid Earth, 123, 2396–2409. https://doi.org/10.1002/2017JB015168</p>
Shear wave splitting measurements used in "Spatio-temporal Analysis of Seismic Anisotropy Associated with the Cook Strait and Kaikoura Earthquake Sequences in New Zealand"
<p>Shear wave splitting measurement used in "Spatio-temporal Analysis of Seismic Anisotropy Associated with the Cook Strait and Kaikoura Earthquake Sequences in New Zealand" is included here. This CSV and XLSX file are part of a paper submitted to GJI in April 2020. A detailed description of the column headers can be found in the MFAST manual, in table 4, at http://mfast-package.geo.vuw.ac.nz/mfast_manual_v2.2.pdf</p>
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