Detecting multidomain magnetic grains in Thellier palaeointensity experiments
By P. Riisager, J. Riisager. 2001
242 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/e48d014158cf22bb2de1df7e108898282107d2f5
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Citations in the corpus
- ArcheoInt: An upgraded compilation of geomagnetic field intensity data for the past ten millennia and its application to the recovery of the past dipole moment (2008, unknown): “…recently been developed to detect multidomain (MD) grains behavior which could bias the intensity determination [e.g., Dunlop and Ozdemir , 1997; Riisager and Riisager , 2001; Krasa et al. , 2003; Yu et al. , 2004; Leonhardt et al. , 2004], this information is not provided in the present…”
- Toward an optimal geomagnetic field intensity determination technique (2004, methodology): “This behavior has been interpreted as indicating the presence of multidomain or vortex remanence state particles [e.g., Riisager et al., 2000, 2002; Riisager and Riisager, 2001; Yu and Dunlop, 2001, 2003; Carvallo et al., 2004; Tauxe and Love, 2003].”
- The application of acceptance criteria to results of Thellier palaeointensity experiments performed on samples with pseudo-single-domain-like characteristics (2003, methodology): “…was chosen to be equal in magnitude and direction to that used to impart the full TRM. Additionally, after each double heating stage, the samples were subjected to further heating and measurement stages to allow pTRM checks and ‘pTRM tail’ checks (Riisager and Riisager, 2001) to be calculated.”
- Reliable absolute palaeointensities independent of magnetic domain state (2006, methodology): “pTRM checks the test for alteration, while pTRM tail checks [15] and additivity checks [16] the test for multidomain behaviour that shows up as convex-down inArai plots.”