The effect of cooling rate on the intensity of thermoremanent magnetization (TRM) acquired by assemblages of pseudo-single domain, multidomain and interacting single-domain grains-Reference-Cited by-同舟云学术

The effect of cooling rate on the intensity of thermoremanent magnetization (TRM) acquired by assemblages of pseudo-single domain, multidomain and interacting single-domain grains

Published:2013-03-30 Issue:3 Volume:193 Page:1239-1249
ISSN:1365-246X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Biggin A. J.,Badejo S.,Hodgson E.,Muxworthy A. R.,Shaw J.,Dekkers M. J.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/article-pdf/193/3/1239/5987205/ggt078.pdf

Reference38 articles.

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3. A thermomagnetic criterion for determining the domain structure of ferrimagnetics;Bol'shakov;Izv. Acad. Sci. USSR Phys. Solid Earth,1979

4. Relationship between median destructive field and remanent coercive forces for dispersed natural magnetite, titanomagnetite and hematite;Dankers;Geophys. J. R. astr. Soc.,1981

5. Magnetic blocking temperatures of single-domain grains during slow cooling;Dodson;J. geophys. Res.,1980

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