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The ups and downs of the TVZ: Geodetic observations of deformation around the Taupo Volcanic Zone, New Zealand
Author(s) -
Hamling I. J.,
Hreinsdóttir S.,
Fournier N.
Publication year - 2015
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.983
H-Index - 232
eISSN - 2169-9356
pISSN - 2169-9313
DOI - 10.1002/2015jb012125
Subject(s) - geology , interferometric synthetic aperture radar , volcano , seismology , sill , subsidence , crust , subduction , geodesy , rift , tectonics , geomorphology , synthetic aperture radar , paleontology , geochemistry , remote sensing , structural basin
The 300 km long Taupo Volcanic Zone (TVZ) formed as a result of back‐arc rifting associated with subduction of the Pacific Plate beneath the Australian Plate, with current extension rates of 8–15 mm yr −1 . Using GPS and interferometric synthetic aperture radar (InSAR) data, collected by the European (ESA) and Japanese (JAXA) space agencies, we present ground deformation observations from 2003 to 2011. Both InSAR and vertical GPS data show widespread subsidence across the central TVZ at rates of up to 20 mm yr −1 . Using simple elastic dislocation models to represent the contraction of a sill like body at 6 km depth, we predict an annual volume change of 0.011–0.016 km 3 beneath the central TVZ. We suggest that the majority of the observed subsidence is a result of the cooling and subsequent contraction of magma within the shallow crust.