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CHARLIER, B. L. A., WILSON, C. J. N., LOWENSTERN, J. B., BLAKE, S., VAN CALSTEREN, P. W., DAVIDSON, J. P. (2005) Magma Generation at a Large, Hyperactive Silicic Volcano (Taupo, New Zealand) Revealed by U–Th and U–Pb Systematics in Zircons. Journal of Petrology, 46 (1) 3-32 doi:10.1093/petrology/egh060

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Reference TypeJournal (article/letter/editorial)
TitleMagma Generation at a Large, Hyperactive Silicic Volcano (Taupo, New Zealand) Revealed by U–Th and U–Pb Systematics in Zircons
JournalJournal of Petrology
AuthorsCHARLIER, B. L. A.Author
WILSON, C. J. N.Author
LOWENSTERN, J. B.Author
BLAKE, S.Author
VAN CALSTEREN, P. W.Author
DAVIDSON, J. P.Author
Year2005 (January)Volume46
Page(s)3-32Issue1
PublisherOxford University Press (OUP)
DOIdoi:10.1093/petrology/egh060Search in ResearchGate
Mindat Ref. ID178062Long-form Identifiermindat:1:5:178062:2
GUID9fd1ff75-e4df-473a-94f9-0016f45aae61
Full ReferenceCHARLIER, B. L. A., WILSON, C. J. N., LOWENSTERN, J. B., BLAKE, S., VAN CALSTEREN, P. W., DAVIDSON, J. P. (2005) Magma Generation at a Large, Hyperactive Silicic Volcano (Taupo, New Zealand) Revealed by U–Th and U–Pb Systematics in Zircons. Journal of Petrology, 46 (1) 3-32 doi:10.1093/petrology/egh060
Plain TextCHARLIER, B. L. A., WILSON, C. J. N., LOWENSTERN, J. B., BLAKE, S., VAN CALSTEREN, P. W., DAVIDSON, J. P. (2005) Magma Generation at a Large, Hyperactive Silicic Volcano (Taupo, New Zealand) Revealed by U–Th and U–Pb Systematics in Zircons. Journal of Petrology, 46 (1) 3-32 doi:10.1093/petrology/egh060
In(2005, January) Journal of Petrology Vol. 46 (1) Oxford University Press (OUP)

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Brown, S. J. A. & Fletcher, I. R. (1999). SHRIMP U–Pb dating of the preeruption growth history of zircons from the 340 ka Whakamaru Ignimbrite, New Zealand: evidence for >250 k.y. magma residence times. Geology27, 1035–1038.
Charlier, B. L. A. (2000). U–Th isotopic constraints on the pre-eruptive dynamics of large-scale silicic volcanism: examples from New Zealand. Ph.D. thesis, The Open University, Milton Keynes.
Charlier, B. L. A., Davidson, J. P. & Wilson, C. J. N. (2003). Generation processes in a high-silica rhyolite as recorded in plagioclase crystals from Taupo volcano, New Zealand. Geophysical Research Abstracts5, abstract 05352.
Dunbar, N. W. & Kyle, P. R. (1993). Lack of volatile gradient in the Taupo plinian–ignimbrite transition: evidence from melt inclusion analysis. American Mineralogist78, 177–184.
Not Yet Imported: Geological Society of America Special Papers - book-chapter : 10.1130/SPE180-p43

If you would like this item imported into the Digital Library, please contact us quoting Journal ID 25243
Lindsay, J. M., Williams, I. S., Ireland, T. R., Smith, I. E. M. & Black, P. M. (1994). Zircon ages in young felsic volcanics and underlying basement in northern New Zealand: implications for rhyolite genesis (abstract). US Geological Survey Circular1107, 196.
Ludwig, K. R. (2002). Isoplot/Ex Version 2.49: a Geochronological Toolkit for Microsoft Excel. Berkeley, CA: Berkeley Chronology Center.
Palmer, K., Mortimer, N., Nathan, S., Isaac, M. J., Field, B. D., Sircombe, K. N., Black, P. M., Bush, S. & Orr, N. W. (1995). Chemical and petrographic analyses of some New Zealand Paleozoic–Mesozoic metasedimentary and igneous rocks. Lower Hutt, New Zealand: Institute of Geological & Nuclear Sciences, Science Report95/16, 1–37.
Not Yet Imported: Geological Society of America Special Papers - book-chapter : 10.1130/SPE180-p5

If you would like this item imported into the Digital Library, please contact us quoting Journal ID 25243
Sutton, A. N. (1995). Evolution of a large silicic magma system: Taupo volcanic centre, New Zealand. Ph.D. thesis, The Open University, Milton Keynes.
Wilson, C. J. N., Charlier, B. L. A., Blake, S. & Sutton, A. N. (2002). Pyroclastic deposits from ca. 64 to 26·5 ka in the Maroa–Taupo area, New Zealand, reflect contemporaneous independent silicic magmatic systems. EOS Transactions, American Geophysical Union83(22), Western Pacific Geophysics Meeting Supplement, Abstract SE 51B-01.


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