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.{{cite book}}: CS1 maint: multiple names: authors list (link)
  • 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. (eds.). 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 (eds.). Encyclopedia of geomagnetism and paleomagnetism. Dordrecht: Springer. pp. 157–158. ISBN 9781402044236.
  • Ravat, D.; Morgan, P.; Lowry, A.R.. (2016). "Geotherms from the temperature-depth–constrained solutions of 1-D steady-state heat-flow equation". Geosphere. 12 (4). Bibcode:2016Geosp..12.1187R. doi:10.1130/GES01235.1.
  • Ravat, Dhananjay (2000). "Curie Temperature (Curie Isotherm)". In Hancock, P.L.; Skinner, B.J. (eds.). Oxford Companion to the Earth. Oxford: Oxford University Press. pp. 202–203.


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