Structural control and origin of volcanism in the Taupo volcanic zone, New Zealand

@article{Cole1990StructuralCA,
  title={Structural control and origin of volcanism in the Taupo volcanic zone, New Zealand},
  author={Jim Cole},
  journal={Bulletin of Volcanology},
  year={1990},
  volume={52},
  pages={445-459}
}
  • J. Cole
  • Published 1 August 1990
  • Geology
  • Bulletin of Volcanology
Taupor volcanic zone (TVZ) is the currently active volcanic arc and back-arc basin of the Taupo-Hikurangi arc-trench system, North Island, New Zealand. The volcanic arc is best developed at the southern (Tongariro volcanic centre) end of the TVZ, while on the eastern side of the TVZ it is represented mainly by dacite volcanoes, and in the Bay of Plenty andesite/dacite volcanoes occur on either side of the Whakatane graben. The back-arc basin is best developed in the central part of the TVZ and… 
Caldera volcanism and rift structure in the Taupo Volcanic Zone, New Zealand
Abstract The Taupo Volcanic Zone (TVZ) is an active continental volcanic arc/back-arc basin in central North Island, New Zealand. It is the youngest area of volcanic activity that extends southwards
Taupo Volcanic Zone and Central Volcanic Region Backarc Structures of North Island, New Zealand
Volcanism in North Island, New Zealand, is related to subduction within the Taupo-Hikurangi arc-trench system. The central volcanic region (CVR) is a wedge-shaped basin, approximately 4 m.y. old,
Petrogenesis of High-K Arc Magmas: Evidence from Egmont Volcano, North Island, New Zealand
Egmont Volcano (Mt Taranaki) is located 140 km west of the INTRODUCTION Taupo Volcanic Zone (TVZ), the principal locus of volcanic activity Egmont Volcano is a 2518 m high stratovolcano (Mt in the
Extensional fault kinematics within the Taupo Volcanic Zone, New Zealand: Soft‐linked segmentation of a continental rift system
Abstract The Taupo Volcanic Zone (TVZ) is a young (<2 Ma) arc‐backarc system in continental crust at the southern end of the Havre Trough characterised by intense volcanism and geothermal activity.
Magma Origin and Evolution of White Island (Whakaari) Volcano, Bay of Plenty, New Zealand
White Island is an active composite stratovolcano in the Bay of of the North Island, the Pacific Plate is being subducted Plenty, New Zealand, that comprises many small volume westwards under the
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References

SHOWING 1-10 OF 61 REFERENCES
Taupo-Rotorua Depression: an ensialic marginal basin of North Island, New Zealand
  • J. W. Cole
  • Geology
    Geological Society, London, Special Publications
  • 1984
Summary New Zealand lies on the boundary between the Pacific and Indian plates. In the vicinity of North Island, oceanic crust of the Pacific plate is subducted obliquely beneath continental crust of
Genesis of lavas of the Taupo Volcanic Zone, North Island, New Zealand
Caldera Volcanoes of the Taupo Volcanic Zone, New Zealand
The Taupo volcanic zone (TVZ) has been active since 2 Ma and has erupted >104 km3 of dominantly rhyolitic magma during the last 1 m.y. Most of the volcanism is concentrated in a 125×60 km area
Evolution of the Taupo-Hikurangi subduction system
Intersection of a marginal basin with a continent: structure and sediments of the Bay of Plenty, New Zealand
Summary West of the Kermadec Trench and Arc, the Havre Trough is an actively spreading, oceanic marginal basin. Bathymetric, magnetic and seismic data indicate that it terminates against the lower
Geodetic strain and the deformational history of the North Island of New Zealand during the late Cainozoic
  • R. Walcott
  • Geology
    Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences
  • 1987
The subduction zone under the east coast of the North Island of New Zealand comprises, from east to west, a frontal wedge, a fore-arc basin, uplifted basement forming the arc and the Central Volcanic
Subduction and back-arc activity at the Hikurangi convergent Margin, New Zealand
The Hikurangi Margin is a region of oblique subduction with northwest-dipping intermediate depth seismicity extending southwest from the Kermadec system to about 42°S. The current episode of
Some Studies of the Geology, Volcanic History, and Geothermal Resources of the Okataina Volcanic Centre, Taupo Volcanic Zone, New Zealand
Okataina Volcanic Centre is the most recently active of the four major rhyolite eruptive centres in the Taupo Volcanic Zone of New Zealand. Within the Centre lies Haroharo Caldera, a complex of
Volcanic hazard assessment for Ruapehu composite volcano, taupo volcanic zone, New Zealand
Ruapehu is a very active andesitic composite volcano which has erupted five times in the past 10 years. Historical events have included phreatomagmatic eruptions through a hot crater lake and two
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