Shear wave velocity variation across the Taupo Volcanic Zone, New Zealand, from receiver function inversion
The Taupo Volcanic Zone (TVZ), New Zealand is a region characterized by very high magma eruption rates and extremely high heat flow, which is manifest in high-temperature geothermal waters. The shear wave velocity structure across the region is inferred using non-linear inversion of receiver functio...
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| Published in | Geophysical journal international Vol. 159; no. 1; pp. 291 - 310 |
|---|---|
| Main Authors | , , |
| Format | Journal Article |
| Language | English |
| Published |
Oxford, UK
Blackwell Publishing Ltd
01.10.2004
Blackwell Science Ltd |
| Subjects | |
| Online Access | Get full text |
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| Abstract | The Taupo Volcanic Zone (TVZ), New Zealand is a region characterized by very high magma eruption rates and extremely high heat flow, which is manifest in high-temperature geothermal waters. The shear wave velocity structure across the region is inferred using non-linear inversion of receiver functions, which were derived from teleseismic earthquake data. Results from the non-linear inversion, and from forward synthetic modelling, indicate low S velocities at ∼6–16 km depth near the Rotorua and Reporoa calderas. We infer these low-velocity layers to represent the presence of high-level bodies of partial melt associated with the volcanism. Receiver functions at other stations are complicated by reverberations associated with near-surface sedimentary layers. The receiver function data also indicate that the Moho lies between 25 and 30 km, deeper than the 15 ± 2 km depth previously inferred for the crust–mantle boundary beneath the TVZ. |
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| AbstractList | SUMMARY
The Taupo Volcanic Zone (TVZ), New Zealand is a region characterized by very high magma eruption rates and extremely high heat flow, which is manifest in high‐temperature geothermal waters. The shear wave velocity structure across the region is inferred using non‐linear inversion of receiver functions, which were derived from teleseismic earthquake data. Results from the non‐linear inversion, and from forward synthetic modelling, indicate low S velocities at ∼6–16 km depth near the Rotorua and Reporoa calderas. We infer these low‐velocity layers to represent the presence of high‐level bodies of partial melt associated with the volcanism. Receiver functions at other stations are complicated by reverberations associated with near‐surface sedimentary layers. The receiver function data also indicate that the Moho lies between 25 and 30 km, deeper than the 15 ± 2 km depth previously inferred for the crust–mantle boundary beneath the TVZ. The Taupo Volcanic Zone (TVZ), New Zealand is a region characterized by very high magma eruption rates and extremely high heat flow, which is manifest in high-temperature geothermal waters. The shear wave velocity structure across the region is inferred using non-linear inversion of receiver functions, which were derived from teleseismic earthquake data. Results from the non-linear inversion, and from forward synthetic modelling, indicate low S velocities at 66-16 km depth near the Rotorua and Reporoa calderas. We infer these low-velocity layers to represent the presence of high-level bodies of partial melt associated with the volcanism. Receiver functions at other stations are complicated by reverberations associated with near-surface sedimentary layers. The receiver function data also indicate that the Moho lies between 25 and 30 km, deeper than the 15 c 2 km depth previously inferred for the crust-mantle boundary beneath the TVZ. The Taupo Volcanic Zone (TVZ), New Zealand is a region characterized by very high magma eruption rates and extremely high heat flow, which is manifest in high-temperature geothermal waters. The shear wave velocity structure across the region is inferred using non-linear inversion of receiver functions, which were derived from teleseismic earthquake data. Results from the non-linear inversion, and from forward synthetic modelling, indicate low S velocities at ∼6–16 km depth near the Rotorua and Reporoa calderas. We infer these low-velocity layers to represent the presence of high-level bodies of partial melt associated with the volcanism. Receiver functions at other stations are complicated by reverberations associated with near-surface sedimentary layers. The receiver function data also indicate that the Moho lies between 25 and 30 km, deeper than the 15 ± 2 km depth previously inferred for the crust–mantle boundary beneath the TVZ. |
| Author | Bibby, H. M. Bannister, S. Bryan, C. J. |
| Author_xml | – sequence: 1 givenname: S. surname: Bannister fullname: Bannister, S. email: Institute of Geological and Nuclear Sciences, PO Box 30368, Lower Hutt 6315, New Zealand. s.bannister@gns.cri.nz, s.bannister@gns.cri.nz organization: Institute of Geological and Nuclear Sciences, PO Box 30368, Lower Hutt 6315, New Zealand. E-mail: s.bannister@gns.cri.nz – sequence: 2 givenname: C. J. surname: Bryan fullname: Bryan, C. J. organization: United States Geological Survey, Vancouver, USA – sequence: 3 givenname: H. M. surname: Bibby fullname: Bibby, H. M. email: Institute of Geological and Nuclear Sciences, PO Box 30368, Lower Hutt 6315, New Zealand. s.bannister@gns.cri.nz, s.bannister@gns.cri.nz organization: Institute of Geological and Nuclear Sciences, PO Box 30368, Lower Hutt 6315, New Zealand. E-mail: s.bannister@gns.cri.nz |
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| Snippet | The Taupo Volcanic Zone (TVZ), New Zealand is a region characterized by very high magma eruption rates and extremely high heat flow, which is manifest in... SUMMARY The Taupo Volcanic Zone (TVZ), New Zealand is a region characterized by very high magma eruption rates and extremely high heat flow, which is manifest... |
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| SubjectTerms | crustal structure receiver functions Taupo Volcanic Zone waveform inversion |
| Title | Shear wave velocity variation across the Taupo Volcanic Zone, New Zealand, from receiver function inversion |
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