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Topic: Takesi Nagata

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	Geomagnetism: Theories of Since 1900
		The principal hope in deep geomagnetic probing is that a knowledge of conductivity will give information on temperature.
		Work on the temperature dependence of the conductivity of mantle material was done by Takesi Nagata in 1937, and was continued by H.
		Coster in 1948, by Harry Hughes in Cambridge and by K. Noritomi in Japan in the mid 1950's.
	www.agu.org /history/mf/articles/Geomag20.html (5907 words)

	DVKcv2000 (Site not responding. Last check: 2007-10-15)
		Johnson, H.P., W. Lowrie and D.V. Kent, 1975, Stability of anhysteretic remanent magnetization in fine and coarse magnetite and maghemite particles, Geophysical Journal of the Royal Astronomical Society, 41, 1-10.
		Kent, D.V., 1975, Post-depositional detrital remanent magnetism in reconstituted deep sea sediment, in Proceedings Takesi Nagata Conference (June 1974, University of Pittsburgh, Pittsburgh), 85-95.
		Kent, D.V. and W. Lowrie, 1975, On the magnetic susceptibility anisotropy of deep sea sediment, Earth and Planetary Science Letters, 28, 1-12.
	www.ldgo.columbia.edu /~polsen/nbcp/dvk.cv1.html (6471 words)

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