3 Works

New Zealand Community Fault Model - version 1.0

Hannu Seebeck, Russ J. Van Dissen, Nicola J. Litchfield, P. M. Barnes, Andy Nicol, Rob M. Langridge, David J. A. Barrell, Pilar Villamor, Susan M. Ellis & Mark S. Rattenbury
Fault models developed by the scientific community aim to provide a consistent and broadly agreed-upon representation of faults in a region for such societally important endeavours as seismic hazard assessment (e.g. national seismic hazard models), strong ground-motion predictions and physics-based fault systems modelling. The New Zealand Community Fault Model (NZ CFM) is a two- and three-dimensional representation of fault zones associated with the New Zealand plate boundary for which Quaternary activity has been established (or...

Te Tai-o-Rēhua – Silent Tsunami: voyage report R/V Tangaroa TAN2205, 17 March – 7 April 2022, Wellington–Wellington

Jess I. T. Hillman, S. J. Watson, Suzanne Bull, Malcolm J. Arnot, A. Pallentin, W. Quinn, E. Spain, Suzi Woelz, S. Coursey, G. Warren, F. Warnke & D. Krylova
This report documents the voyage objectives, outcomes and preliminary results of the GNS-Science-led R/V Tangaroa voyage TAN2205, which took place from 15 March to 7 April 2022 in the eastern Tasman Sea (Deepwater Taranaki Basin). The over-arching aim of the voyage was to acquire new information to help progress our understanding of the link between submarine landslides and tsunami in the Tasman Sea. The voyage is part of the 2021 Ministry of Business, Innovation &...

'Geologic Champagne' voyage report R/V Tangaroa TAN2006: 26 June - 17 July 2020, Wellington-Wellington

Ingo A. Pecher, Jess I. T. Hillman, Bryan W. Davy, A. R. Gorman, Suzi Woelz, D. Andrew, L. Boettger, A. Dalbeth, P. Gerring, J. Hoffman, A. Macnaughtan, P. Oluwunmi, W. Quinn, A. Shorrock & M. Tankersley
Tangaroa voyage TAN2006 took place from 26 June – 17 July 2020, with an unscheduled port call in Wellington from 29 June – 1 July due to equipment problems. The voyage objectives focused on geophysical studies of seafloor pockmarks on the Chatham Rise, as well as possible pockmarks and contourite deposits in the Bounty Trough. We acquired ~800 km of 2D seismic data, ~500 km of which were in a dense grid designed for high-resolution...

Registration Year

  • 2022
    3

Resource Types

  • Text
    3

Affiliations

  • GNS Science
    3
  • National Institute of Water and Atmospheric Research
    3
  • University of Auckland
    2
  • Victoria University of Wellington
    1
  • University of Otago
    1
  • University of Canterbury
    1