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Beresford, S. W., Cole, J. W. (2000) Kaingaroa Ignimbrite, Taupo Volcanic Zone, New Zealand: Evidence for asymmetric caldera subsidence of the Reporoa Caldera. New Zealand Journal of Geology and Geophysics, 43 (3) 471-481 doi:10.1080/00288306.2000.9514903

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Reference TypeJournal (article/letter/editorial)
TitleKaingaroa Ignimbrite, Taupo Volcanic Zone, New Zealand: Evidence for asymmetric caldera subsidence of the Reporoa Caldera
JournalNew Zealand Journal of Geology and Geophysics
AuthorsBeresford, S. W.Author
Cole, J. W.Author
Year2000 (September)Volume43
Issue3
PublisherInforma UK Limited
DOIdoi:10.1080/00288306.2000.9514903Search in ResearchGate
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Mindat Ref. ID258228Long-form Identifiermindat:1:5:258228:7
GUID0
Full ReferenceBeresford, S. W., Cole, J. W. (2000) Kaingaroa Ignimbrite, Taupo Volcanic Zone, New Zealand: Evidence for asymmetric caldera subsidence of the Reporoa Caldera. New Zealand Journal of Geology and Geophysics, 43 (3) 471-481 doi:10.1080/00288306.2000.9514903
Plain TextBeresford, S. W., Cole, J. W. (2000) Kaingaroa Ignimbrite, Taupo Volcanic Zone, New Zealand: Evidence for asymmetric caldera subsidence of the Reporoa Caldera. New Zealand Journal of Geology and Geophysics, 43 (3) 471-481 doi:10.1080/00288306.2000.9514903
In(2000, September) New Zealand Journal of Geology and Geophysics Vol. 43 (3) Informa UK Limited

See Also

These are possibly similar items as determined by title/reference text matching only.

Beresford, S. W., Cole, J. W. (2000) Kawerau Ignimbrite: A 0.24 Ma ignimbrite erupted from the Okataina caldera complex, Taupo Volcanic Zone, New Zealand. New Zealand Journal of Geology and Geophysics, 43 (1) 109-115 doi:10.1080/00288306.2000.9514873
Beresford, S. W., Cole, J. W., Weaver, S. D. (2000) Weak chemical and mineralogical zonation in the Kaingaroa Ignimbrite, Taupo Volcanic Zone, New Zealand. New Zealand Journal of Geology and Geophysics, 43 (4) 639-650 doi:10.1080/00288306.2000.9514914
Hildyard, S. C., Cole, J. W., Weaver, S. D. (2000) Tikorangi Ignimbrite: A 0.89 Ma mixed andesiteā€rhyolite ignimbrite, Matahana Basin, Taupo Volcanic Zone, New Zealand. New Zealand Journal of Geology and Geophysics, 43 (1) 95-107 doi:10.1080/00288306.2000.9514872
Bannister, Stephen, Melhuish, Anne (1997) Seismic scattering and reverberation, Kaingaroa plateau, Taupo Volcanic Zone, New Zealand. New Zealand Journal of Geology and Geophysics, 40 (3) 375-381 doi:10.1080/00288306.1997.9514768
Cole, J. W. (1979) Structure, petrology, and genesis of Cenozoic volcanism, Taupo Volcanic Zone, New Zealandā€”a review. New Zealand Journal of Geology and Geophysics, 22 (6) 631-657 doi:10.1080/00288306.1979.10424173
Briggs, R. M., Fulton, B. W. J. (1990) Volcanism, structure, and petrology of the Whiritoa-Whangamata coastal section, Coromandel Volcanic Zone, New Zealand: Facies model evidence for the Tunaiti caldera. New Zealand Journal of Geology and Geophysics, 33 (4) 623-633 doi:10.1080/00288306.1990.10421380
Bailey, Roy A., Carr, R. Garry (1994) Physical geology and eruptive history of the Matahina Ignimbrite, Taupo Volcanic Zone, North Island, New Zealand. New Zealand Journal of Geology and Geophysics, 37 (3) 319-344 doi:10.1080/00288306.1994.9514624
Milner, D.M, Cole, J.W, Wood, C.P (2003) Mamaku Ignimbrite: a caldera-forming ignimbrite erupted from a compositionally zoned magma chamber in Taupo Volcanic Zone, New Zealand. Journal of Volcanology and Geothermal Research, 122 (3) 243-264 doi:10.1016/s0377-0273(02)00504-8
Healy, J. (1964) Volcanic mechanisms in the Taupo Volcanic Zone, New Zealand. New Zealand Journal of Geology and Geophysics, 7 (1) 6-23 doi:10.1080/00288306.1964.10420154
Ewart, A. (1965) Mineralogy and Petrogenesis of the Whakamaru Ignimbrite in the Maraetai area of the Taupo volcanic zone, New Zealand. New Zealand Journal of Geology and Geophysics, 8 (4) 611-679 doi:10.1080/00288306.1965.10423194
D., Milner, J., Cole, C., Wood (2002) Asymmetric, multiple-block collapse at Rotorua Caldera, Taupo Volcanic Zone, New Zealand. Bulletin of Volcanology, 64 (2). 134-149 doi:10.1007/s00445-001-0191-0
 
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