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Volume 2, issue 2
Solid Earth, 2, 259–270, 2011
https://doi.org/10.5194/se-2-259-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
Solid Earth, 2, 259–270, 2011
https://doi.org/10.5194/se-2-259-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Nov 2011

Research article | 21 Nov 2011

Paleointensities on 8 ka obsidian from Mayor Island, New Zealand

A. Ferk et al.
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Cited articles  
Bowles, J., Gee, J. S., Kent, D. V., Bergmanis, E., and Sinton, J.: Cooling rate effects on paleointensity estimates in submarine basaltic glass and implications for dating young flows, Geochem. Geophys. Geosys., 6, Q07002, https://doi.org/10.1029/2004GC000900, 2005.
Buck, M. D., Briggs, R. M., and Nelson, C. S.: Pyroclastic deposits and volcanic history of Mayor Island, N. Z. J. Geol. Geophys., 24, 449–4667, 1981.
Coe, R. S.: The determinations of paleointensities of the Earth's magnetic field with emphasis on mechanisms which could cause non-ideal behavior in Thellier's method, Geomag. Geoelec., 19, 157–179, 1967.
Coe, R. S., Grommé, S., and Mankinen, E. A.: Geomagnetic paleointensities from radiocarbon-dated lava flows on Hawaii and the question of the Pacific nondipole low, J. Geophys. Res., 83, 1740–1756, 1978.
Cottrell, R. D. and Tarduno, J. A.: Geomagnetic paleointensity derived from single plagioclase crystals, Earth Planet. Sci. Lett., 169, 1–5, 1999.
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