The New Zealand primary site exhibits a wide range of fault slip and volcanic phenomena with significant variation along-strike in a small, compact setting. Excellent exhumed exposures of arc crust and accretionary prism, a zone of active subduction initiation, and significant new government investments in onshore and offshore scientific infrastructure make New Zealand an exciting site for GeoPRISMS research. From north to south, the New Zealand primary site includes the Puysegur Ridge (subduction initiation), Puysegur Trench (subduction), Fiordland (exhumed arc crust), Hikurangi Trench (subduction), the Taupo Volcanic Zone (arc and rift volcanism), the southern Kermadec Arc (subduction), and the Havre Trough (back-arc rifting).
Click on each theme below to see current projects and some remarks on that theme from the GeoPRISMS Implementation Plan.
Examples of outstanding research questions for the New Zealand primary site include:
- What are the geological, geochemical, and geophysical responses to subduction initiation and early arc evolution and how to they affect subduction zone formation?
- What controls the along-strike transition from a locked subduction interface (southern Hikurangi) to a largely creeping interface (northern Hikurangi)? What controls the spatial limits of the seismogenic zone and the location and character of slow slip events?
- How to Quaternary eustacy, structural deformation, and climate change influence sediment dispersal and sequence architecture in forearc basins?
- What are the magma transport pathways through the crust, and respective contributions of subducted sediments and crustal assimilation along- and across-strike of the arc?
- How do rifting and spreading, and the spatial and temporal variation of magmatism, relate to the nature of slab-derived fluid-to-melt and the rheology of the mantle wedge?
Further information about these topics, a summary of existing datasets and infrastructure investments in New Zealand, and critical research efforts for GeoPRISMS studies can be found in Section 2.4 of the GeoPRISMS Implementation Plan.
An implementation planning workshop was held for the New Zealand Primary Site in Wellington, New Zealand on 14-16 April, at Te Papa Museum. There were 170 participants from ten different countries, demonstrating the excellent opportunities for international collaboration at this primary site. The large number of participants and high-quality white papers submitted (38 white papers – more than for any of the other GeoPRISMS primary site workshops) reflected the high level of enthusiasm among both the US and international subduction zone community for future studies in New Zealand. The workshop consisted of a number of keynote and invited talks, and break-out sessions to discuss and prioritize the main scientific objectives and most suitable GeoPRISMS goals. Four geographic regions emerged as focus areas where GeoPRISMS topics could be well addressed:
- The Puysegur Trench
- The Hikurangi Subduction Margin
- The Taupo Volcanic Zone
- The Kermadec Arc
The New Zealand IP has been updated based on the outcomes of the workshop and is available for download.
2014
- Workshop to cultivate and coordinate GeoPRISMS studies of the Hikurangi subduction margin | AGU Fall Meeting, Dec 14, 2014
- Mini-Workshop for the South Island, New Zealand Primary Site coordination | AGU Fall Meeting, Dec 14, 2014
2013
- Kermadec Arc-Havre Trough Planning Mini-workshop | AGU Fall Meeting Dec 8, 2013
- Planning Workshop for the New Zealand Primary Site | Wellington, NZ April 15-17, 2013
2011
- SCD Implementation Workshop | Bastrop, TX, January 5-7, 2011
- IODP workshop on using ocean drilling to unlock the secrets of slow-slip events | Gisborne, NZ, Aug 1-5, 2011, Gisborne, New Zealand
New Zealand
- HT-RESIST Hikurangi Trench Regional Electromagnetic Survey to Image the Subduction Thrust
- SISIE: South Island Subduction Initiation Experiment
- Assessing changes in the state of a magma storage system over caldera-forming eruption cycles, a case study at Taupo Volcanic Zone, New Zealand
- Sizing up the Taniwha: Seismogenesis at Hikurangi Integrated Research Experiment (SHIRE)
- Hikurangi Ocean Bottom Investigation of Tremor and Slow Slip (HOBITSS) – Revealing the environment of shallow slow slip
- IODP tackles the Hikurangi Margin of New Zealand with two drilling expeditions to unlock the secrets of slow-slip events
- The NZ3D Experiment – Adding a new dimension for understanding slow slip events
- Volatile cycling through the Hikurangi forearc, New Zealand
- Probing the nature of the Hikurangi margin hydrogeologic system
- Slow slip and future earthquake potential in New Zealand and Cascadia
- Revealing the secrets of the New Zealand GeoPRISMS Primary Site
- HOBITSS Hikurangi Ocean Bottom Investigation of Tremor and Slow Slip
- Report: South Island, New Zealand primary site coordination mini-workshop
- Report: Workshop to cultivate and coordinate GeoPRISMS studies of the Hikurangi subduction margin
- IODP Workshop on Using Ocean Drilling to Unlock the Secrets of Slow Slip Events
- The New Zealand Primary Site Implementation Planning Workshop Report
- Report: Kermadec Arc-Havre Trough Planning Mini-Workshop
SCD
- E-FIRE Field Institute Alps Summer 2017 | Erro Tobbio
- E-FIRE Field Institute Alps Summer 2017 | Voltri Massif
- E-FIRE Field Institute Alps Summer 2017 | Schistes Lustrés
- E-FIRE Field Institute Alps Summer 2017 | Lago di Cignana
- HT-RESIST Hikurangi Trench Regional Electromagnetic Survey to Image the Subduction Thrust
- Putting the “Community” in the Alaska Amphibious Community Seismic Experiment (AACSE): Alaska Peninsula and Western Gulf of Alaska, Summer 2018
- SISIE: South Island Subduction Initiation Experiment
- Assessing changes in the state of a magma storage system over caldera-forming eruption cycles, a case study at Taupo Volcanic Zone, New Zealand
- Sizing up the Taniwha: Seismogenesis at Hikurangi Integrated Research Experiment (SHIRE)
- Hikurangi Ocean Bottom Investigation of Tremor and Slow Slip (HOBITSS) – Revealing the environment of shallow slow slip
- IODP tackles the Hikurangi Margin of New Zealand with two drilling expeditions to unlock the secrets of slow-slip events
- The NZ3D Experiment – Adding a new dimension for understanding slow slip events
- Volatile cycling through the Hikurangi forearc, New Zealand
- Probing the nature of the Hikurangi margin hydrogeologic system
- Slow slip and future earthquake potential in New Zealand and Cascadia
- Revealing the secrets of the New Zealand GeoPRISMS Primary Site
- ExTerra Field Institute and Research Endeavor: Western Alps, Summer 2017
- Magnetotelluric and Seismic Investigation of Arc Melt Generation, Delivery, and Storage beneath Okmok Volcano
- Imaging Magma Under Mount St. Helens with Geophysical and Petrologic Methods
- Report: The Subduction Zone Observatory Workshop
