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- W2010697718 abstract "The onshore Taupo Volcanic Zone (New Zealand) is a region of vigorous, and relatively well studied, geothermalism and hydrothermalism distributed at 20 known sites. Within the offshore extension of the Taupo Volcanic Zone, new data acquired in 1988 and 1989, and a review of survey data since 1966 has delineated three main areas of submarine hydrothermal activity (SHA) on the Bay of Plenty continental shelf. Of these, the most intense and extensive area of SHA is associated with the active late Quaternary faulting of the offshore Whakatane Graben. Within this latter area, there are four major hydrothermal vent sites; the previously reported Calypso vent site, and three others newly located. Three distinct plume forms are recognisable within the water-column, and are related to the state of buoyancy of the hydrothermal fluid, although the character of the plume can change in the vertical since the overlying water mass is density stratified. Some SHA has proved ephemeral over a 22 year period which is here related to a cycle of conduit opening driven by secular extension, and conduit collapse and closure caused by seismic shocks. Mathematical modelling (phase-plane analysis) of the hydrothermal plumes provides a method of analyzing plume forms from known initial parameters." @default.
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- W2010697718 date "1994-11-01" @default.
- W2010697718 modified "2023-10-17" @default.
- W2010697718 title "Submarine hydrothermal activity within the offshore Taupo Volcanic Zone, Bay of Plenty continental shelf, New Zealand" @default.
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- W2010697718 doi "https://doi.org/10.1016/0278-4343(94)90083-3" @default.
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