View source for Physics:Paleointensity

In [[Physics:Geomagnetism|geomagnetism]], '''paleointensity''' (or palaeointensity) is the study of changes in the strength of the geomagnetic field over Earth's history. Émile and Odette Thellier were the first to make laboratory measurements to determine the strength of the ancient field responsible for producing remanent magnetization in a rock or archeological artifacts.<ref>Thellier, E. & Thellier, O. (1959). Sur l'intensité du champ magnétique terrestre dans le passé historique et géologique. Ann. Geophys., 15, 285-376.</ref>
== Absolute paleointensity methods ==
Absolute paleointensity determinations involve measurements that attempt to quantify the past field strength that produced a magnetization in a rock or other material that has cooled from a high temperature. Most of these methods involve progressively removing the [[Physics:Natural remanent magnetization|natural remanent magnetization]] (NRM) by thermal demagnetization and replacing it with a laboratory [[Physics:Thermoremanent magnetization|thermoremanent magnetization]] given in a magnetic field of known strength and direction.<ref>Tauxe, L, Banerjee, S.K., Butler, R.F. and van der Voo R, Essentials of Paleomagnetism, 4th Web Edition, 2016, Chapter 10.</ref> Various methods for measuring absolute paleointensity include:
* Thellier-Thellier method<ref>Thellier, E. & Thellier, O. (1959). Sur l'intensité du champ magnétique terrestre dans le passé historique et géologique. Ann. Geophys., 15, 285-376.</ref>
* Shaw method<ref>Shaw, J. (1974). A new method of determining the magnitude of the paleomagnetic field application to 5 historic lavas and five archeological samples. Geophys. J. R. Astr. Soc., 39, 133–141.</ref> 
* Coe method<ref>Coe, R. S. (1967). The determination of paleo-intensities of the Earth’s magnetic field with emphasis on mechanisms which could cause non-ideal behavior in Thellier’s method. J. Geomag. Geoelectr., 19, 157–178.</ref>
* Athermal paleointensity methods

== Relative paleointensity ==
Relative paleointensity determinations are often used in materials that may be destroyed or strongly altered during heating, such as lake and marine sediments.<ref>Levi, S., & Banerjee, S. K. (1976). On the possibility of obtaining relative paleointensities from lake sediments. Earth and Planetary Science Letters, 29(1), 219-226.</ref> A measure of relative changes in paleointensity may be obtained by normalizing the NRM by a factor that represents the concentration of magnetic grains in a sample, such as the anhysteretic remanent magnetization.  

==References==
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[[Category:Geomagnetism]]
[[Category:Paleomagnetism]]
[[Category:Earth sciences]]

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