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
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- {{cite book|last1=Herrero-Bervera|first1=Emilio|last2=Acton|first2=Gary|last3=Krasa|first3=David|last4=Rodriguez|first4=Sedelia|last5=Dekkers|first5=Mark J.|chapter=Rock magnetic characterization through an intact sequence of oceanic crust, IODP hole 1256D |editor-first1=Eduard |editor-last1=Petrovský |editor-first2=David |editor-last2=Ivers |editor-first3=T. |editor-last3=Harinarayana |title=The earth's magnetic interior|date=2011|publisher=Springer|location=Dordrecht|isbn=9789400703230|pages=153–168}}
- {{cite encyclopedia|first=Mita |last=Rajaram |title=Depth to Curie temperature|editor-last1=Gubbins|editor-first1=David|editor-last2=Herrero-Bervera|editor-first2=Emilio|encyclopedia=Encyclopedia of geomagnetism and paleomagnetism|date=2007|publisher=Springer|location=Dordrecht|isbn=9781402044236|pages=157–158}}
- {{cite journal |last1=Ravat |first1=D. |last2=Morgan |first2=P. |last3=Lowry |first3=A.R.. |title=Geotherms from the temperature-depth–constrained solutions of 1-D steady-state heat-flow equation |journal=Geosphere |volume=12 |issue=4 |date=2016 |doi=10.1130/GES01235.1 |bibcode=2016Geosp..12.1187R |doi-access=free }}
- {{cite encyclopedia|first=Dhananjay |last=Ravat |title=Curie Temperature (Curie Isotherm)|editor-last1=Hancock|editor-first1=P.L.|editor-last2=Skinner|editor-first2=B.J.|encyclopedia=Oxford Companion to the Earth|date=2000|publisher=Oxford University Press|location=Oxford|pages=202–203}}
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