Theory of partial thermoremanent magnetization in multidomain grains: 1. Repeated identical barriers to wall motion (single microcoercivity)-Reference-Cited by-同舟云学术

Theory of partial thermoremanent magnetization in multidomain grains: 1. Repeated identical barriers to wall motion (single microcoercivity)

Published:1994-05-10 Issue:B5 Volume:99 Page:9005-9023
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Dunlop David J.,Xu Song

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jb/v099/iB05/93JB02566/93JB02566.pdf

Reference31 articles.

1. Thermomagnetic criteria for ferrimagnetic domain structure;Bolshakov;Izv. Akad. Nauk SSSR, Ser. Fiz. Zemli,1979

2. TRM and its variation with grain size;Day;J. Geomagn. Geoelectr.,1977

3. Theory of the magnetic viscosity of lunar and terrestrial rocks;Dunlop;Rev. Geophys.,1973

4. Field dependence of magnetic blocking temperature: Analog tests using coercive force data;Dunlop;J. Geophys. Res.,1982

5. On the demagnetizing energy and demagnetizing factor of a multidomain ferromagnetic cube;Dunlop;Geophys. Res. Lett.,1983

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