Linear and nonlinear Thellier paleointensity behavior of natural minerals

Author:

Dunlop David J.

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

Reference70 articles.

1. Alternating field characteristics of pseudo-single-domain (2–14 μm) and multidomain magnetite;Bailey;Earth Planet. Sci. Lett.,1983

2. The application of acceptance criteria to results of Thellier palaeointensity experiments performed on samples with pseudo-single-domain characteristics;Biggin;Phys. Earth Planet. Inter.,2003

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

4. Theoretical single-domain grain-size range in magnetite and titanomagnetite;Butler;J. Geophys. Res.,1975

5. Interacting vs. non-interacting single domain behavior in natural and synthetic samples;Cisowski;Phys. Earth Planet. Inter.,1981

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