Abstract:<p><b>In this thesis, the factors controlling seismic velocity at the log scale (less than a metre) were explored and this knowledge used to interpret seismic velocity images at the field scale (greater than 200 m) obtained via seismic tomography at two geothermal fields in the Taupō Volcanic Zone in New Zealand; the Ngatamariki and Rotokawa fields. Seismic velocity imaging has the potential to provide valuable insights into geothermal reservoirs that can be used for well targeting, resource manage… Show more
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