Curie depth

In geophysics, the Curie depth is the depth at which rocks in a specific geographical area encounter the Curie temperature. This depth can be approximated from aeromagnetic survey data through spectral analysis or forward modeling.

References

• Artemieva, Irina (2011). The Lithosphere: An Interdisciplinary Approach. Cambridge University Press. ISBN 9781139504461.
• Cull, G.R. Beardsmore, J.P. (2001). "Curie depth". Crustal heat flow a guide to measurement and modelling. Cambridge, UK: Cambridge University Press. pp. 70–71. ISBN 9780521797030.
• Herrero-Bervera, Emilio; Acton, Gary; Krasa, David; Rodriguez, Sedelia; Dekkers, Mark J. (2011). "Rock magnetic characterization through an intact sequence of oceanic crust, IODP hole 1256D". In Petrovský, Eduard; Ivers, David; Harinarayana, T. The earth's magnetic interior. Dordrecht: Springer. pp. 153–168. ISBN 9789400703230.
• Rajaram, Mita (2007). "Depth to Curie temperature". In Gubbins, David; Herrero-Bervera, Emilio. Encyclopedia of geomagnetism and paleomagnetism. Dordrecht: Springer. pp. 157–158. ISBN 9781402044236.