Stephen Bannister, Edward A. Bertrand, Geoff Kilgour, Grant Caldwell, Isabelle Chambefort, Wiebke Heise, Sandra Bourguignon

The Taupo Volcanic Zone (TVZ) in New Zealand is a region of highly pro-
ductive Quaternary volcanism and very large hydrothermal heat flux. Here
we investigate the upper- and mid-crustal seismic velocity structure of a
region within the central, rhyolitic part of the TVZ encompassing the high-
temperature geothermal systems Mokai, Wairakei, Ng¯a Tamariki, Orakei Korako, Te Kopia and Rotokawa. Using double-difference tomographic inversion of local earthquake data we derive 3-D models of P-wave velocity (Vp) and the P- to S-wave velocity ratio (Vp/Vs) for the subsurface. Both high (> 6.0 km/s) and low (< 5.5 km/s) Vp heterogeneities are seen in the mid-crust between 5 and 11 km depth. Regions with high Vp are interpreted to indicate the presence of solidified, more mafic, material within an otherwise quartzo-feldspathic crust, while regions with low Vp values are inferred to represent bodies of crystal-rich low-melt-fraction magma with a low melt fraction.
Using the new 3-D velocity model we then relocated ∼9100 earthquakes
recorded between 2009 and 2022, using EQTransformer to determine P-
and S -phase arrival times. The relocated seismicity is strongly clustered,
including in the vicinity of some of the geothermal systems (e.g. Wairakei
and Rotokawa) where fluid is currently being extracted for electric-power
production. Mid-crustal seismicity is also observed west of the Wairakei
geothermal field, as well as along the south-eastern margin of the Ngakuru
graben (a region of active surface faulting and extension) and on the western margin of the Whakamaru caldera. The depth distribution of the highest-quality hypocentres shows that 90% of the seismicity at Rotokawa geothermal field occurs at depths shallower than 5.1 km, consistent with a shallow brittle-ductile transition and the presence of a cooling pluton beneath Rotokawa seen in magnetotelluric data