Curie depth
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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. It is thought that the subduction of structures can alter the Curie depth of Earth's crust in the surrounding region. Example of this is the subduction of the Juan Fernández Ridge under north-central Chile, a chain of extinct volcanoes on the Nazca Plate which depresses the Curie depth to 39 km northeast of Valparaíso compared with Curie depth ranges from 12 km in the area of Ovalle and Illapel further north.[1]
References
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{{cite book}}: CS1 maint: multiple names: authors list (link) - Page Module:Citation/CS1/styles.css has no content.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.
- Page Module:Citation/CS1/styles.css has no content.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.
- Page Module:Citation/CS1/styles.css has no content.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.
- Page Module:Citation/CS1/styles.css has no content.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.
