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Scott, J.M., Turnbull, I.M., Auer, A., Palin, J.M. (2013) The sub-Antarctic Antipodes Volcano: a B0.5 Ma HIMU-like Surtseyan volcanic outpost on the edge of the Campbell Plateau, New Zealand. New Zealand Journal of Geology and Geophysics.

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Year2013
Original EntryScott, J.M., Turnbull, I.M., Auer, A., Palin, J.M. (2013) The sub-Antarctic Antipodes Volcano: a B0.5 Ma HIMU-like Surtseyan volcanic outpost on the edge of the Campbell Plateau, New Zealand. New Zealand Journal of Geology and Geophysics.
Mindat Ref. ID16084511Long-form Identifiermindat:1:5:16084511:8
GUIDd5c4bfae-6273-4ee0-8d79-379d25069e7a
Full ReferenceScott, J.M., Turnbull, I.M., Auer, A., Palin, J.M. (2013) The sub-Antarctic Antipodes Volcano: a B0.5 Ma HIMU-like Surtseyan volcanic outpost on the edge of the Campbell Plateau, New Zealand. New Zealand Journal of Geology and Geophysics.
Plain TextScott, J.M., Turnbull, I.M., Auer, A., Palin, J.M. (2013) The sub-Antarctic Antipodes Volcano: a B0.5 Ma HIMU-like Surtseyan volcanic outpost on the edge of the Campbell Plateau, New Zealand. New Zealand Journal of Geology and Geophysics.

Locality Pages

LocalityCitation Details
Antipodes Islands, New Zealand Outlying Islands, New Zealand

Mineral Occurrences

LocalityMineral(s)
Antipodes Islands, New Zealand Outlying Islands, New Zealandⓘ Basalt, ⓘ Clinopyroxene Subgroup, ⓘ Fayalite-Forsterite Series, ⓘ Feldspar Group, ⓘ Gabbro, ⓘ Glass, ⓘ Kaersutite, ⓘ Peat, ⓘ Plagioclase, ⓘ Scoria, ⓘ Trachyandesite, ⓘ Tuff, ⓘ Zircon

See Also

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

Scott, J.M., Turnbull, Sagara, M.W., Tulloch, A.J., Waight, T.E., Palin, J.M. (2015) Geology and geochronology of the Sub-Antarctic Snares Islands/Tini Heke, New Zealand. New Zealand Journal of Geology and Geophysics.
Scott, JM, Turnbull, IM, Auer, A, Palin, JM (2013) The sub-Antarctic Antipodes Volcano: a <0.5 Ma HIMU-like Surtseyan volcanic outpost on the edge of the Campbell Plateau, New Zealand. New Zealand Journal of Geology and Geophysics, 56 (3) 134-153 doi:10.1080/00288306.2013.802246
Scott, J.M., Turnbull, I.M. (2019) Geology of New Zealand’s Sub-Antarctic Islands. New Zealand Journal of Geology and Geophysics, 62(2566), 1-27.
Scott, JM, Turnbull, IM, Sagar, MW, Tulloch, AJ, Waight, TE, Palin, JM (2015) Geology and geochronology of the Sub-Antarctic Snares Islands/Tini Heke, New Zealand. New Zealand Journal of Geology and Geophysics, 58 (2) 202-212 doi:10.1080/00288306.2015.1023810
Scott, J., Turnbull, I. (2019) Geology of New Zealand’s Sub-Antarctic Islands. New Zealand Journal of Geology and Geophysics, 62(2566), 1-27.
Scott, James M., Turnbull, Ian M. (2019) Geology of New Zealand’s Sub-Antarctic Islands. New Zealand Journal of Geology and Geophysics, 62 (3) 291-317 doi:10.1080/00288306.2019.1600557
Adams, C.J., Morris, P.A., Beggs, J.M. (1979) Age and correlation of volcanic rocks of Campbell Island and Metamorphic basement of the Campbell Plateau, South-west Pacific. New Zealand Journal of Geology and Geophysics, 22:6, 679-691.
Ritchie, D.D., Turnbull, I.M. (1985) Cenozoic sedimentary rocks at Carnley Harbour, Auckland Islands,Campbell Plateau. New Zealand Journal of Geology and Geophysics, 28 (1) 23-41 doi:10.1080/00288306.1985.10422274
Adams, C.J., Morris, P.A., Beggs, J.M. (1979) Age and correlation of volcanic rocks of Campbell Island and Metamorphic basement of the Campbell Plateau, South-west Pacific. New Zealand Journal of Geology and Geophysics, 22(6), 679-691. doi.org/10.1080/00288306.1979.10424176
Scott, J.M., Borcovsky, D.A., Palin, J.M., Toy, V.G. (2014) Localisation of deformation in the thermal contrast at a granite batholith margin, New Zealand. Journal of Structural Geology, 64. 149-163 doi:10.1016/j.jsg.2013.07.013
Scott, J. M., Turnbull, I. M., Ewing, T. A., Allibone, A. H., Palin, J. M., Cooper, A. F. (2008) Petrology and geochronology of the volcaniclastic and volcanogenic Mesozoic Loch Burn Formation in eastern Fiordland, New Zealand. New Zealand Journal of Geology and Geophysics, 51 (2) 89-103 doi:10.1080/00288300809509852
 
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