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Curie Temperature

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Encyclopedia of Solid Earth Geophysics

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

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Curie point

The critical temperature above which any material loses its permanent magnetism.

A rock containing magnetic minerals loses its permanent magnetism when heated up to reach a critical temperature. This is the Curie temperature or Curie point, ϑ c , above which the rock is paramagnetic. On the atomic level, below ϑ c , the magnetic moments are aligned in their respective domains and even a weak external field results in a net magnetization. As the temperature increases to ϑ c and above, however, fluctuations due to the increase in thermal energy destroy that alignment.

Strongly magnetic minerals are all of ferrimagnetic type, in which neighboring magnetic moments are aligned antiparallel, as in antiferromagnetism, but unequal numbers or strengths give a net magnetization. Among them, magnetite, one of the members of the titanomagnetite solid-solution series, is the most important magnetic mineral to geophysical studies of crustal rocks (Stacey, 1992). There are many...

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Bibliography

  • Blakely, R. J., 1996. Potential Theory in Gravity and Magnetic Applications. Cambridge: Cambridge University Press.

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  • Chiozzi, P., Matsushima, J., Okubo, Y., Pasquale, V., and Verdoya, M., 2005. Curie-point depth from spectral analysis of magnetic data in central-southern Europe. Physics of the Earth and Planetary Interiors, 152, 267–276.

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  • Hunt, C. P., Moskowitz, B. M., and Banerjee, S. K., 1995. Magnetic properties of rocks and minerals. In Ahens, T. J. (ed.), Rock Physics and Phase Relations: A Handbook of Physical Constants. Washington: American Geophysical Union, pp. 189–204.

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  • Stacey, F. D., 1992. Physics of the Earth. Brisbane: Brookfield Press.

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Correspondence to Vincenzo Pasquale .

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© 2011 Springer Science+Business Media B.V.

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Pasquale, V. (2011). Curie Temperature. In: Gupta, H.K. (eds) Encyclopedia of Solid Earth Geophysics. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-8702-7_109

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