Fluid flow associated with silicic lava domes and faults, Ohaaki hydrothermal field, New Zealand
- 1 July 2011
- journal article
- Published by Elsevier BV in Journal of Volcanology and Geothermal Research
- Vol. 204 (1-4), 12-26
- https://doi.org/10.1016/j.jvolgeores.2011.05.002
Abstract
No abstract availableKeywords
This publication has 39 references indexed in Scilit:
- Dike propagation in volcanic edifices: Overview and possible developmentsTectonophysics, 2009
- A geometric model of fault zone and fault rock thickness variationsJournal of Structural Geology, 2009
- Control of magma flow in dykes on cyclic lava dome extrusionGeophysical Research Letters, 2007
- Ohaaki reservoir chemistry: characteristics of an arc-type hydrothermal system in the Taupo Volcanic Zone, New ZealandJournal of Volcanology and Geothermal Research, 2002
- The detection of concealed faults in the Ofanto Basin using the correlation between soil-gas fracture surveysTectonophysics, 1999
- Vegetation change along a geothermal stress gradient at the Te Kopia steamfieldJournal of the Royal Society of New Zealand, 1997
- Fault zone architecture and permeability structureGeology, 1996
- Geophysical evidence on the structure of the Taupo Volcanic Zone and its hydrothermal circulationJournal of Volcanology and Geothermal Research, 1995
- Structural control and origin of volcanism in the Taupo volcanic zone, New ZealandBulletin of Volcanology, 1990
- Structure and eruptive history of the Tarawera Volcanic ComplexNew Zealand Journal of Geology and Geophysics, 1970