Analysis of isothermal remanent magnetization acquisition curves using the expectation-maximization algorithm
By D. Heslop, M. Dekkers, P. Kruiver, I. V. Oorschot. 2002
278 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/4301e4b40ff7143e7bb6bfb704fe17939fcc6725
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Citations in the corpus
- Mechanism of the magnetic susceptibility enhancements of the Chinese loess (2004, unknown): “More recent mathematical ‘‘unmixing’’ techniques involve the separation of coercivity fractions from IRM acquisition curves or alternating field (AF) demagnetization curves [e.g., Robertson and France, 1994; Stockhausen, 1998; Kruiver et al., 2001; Heslop et al., 2002; Egli, 2003].”
- Understanding fine magnetic particle systems through use of first‐order reversal curve diagrams (2014, methodology): “In this regard, interpretation of IRM acquisition curves has been significantly enhanced by routine use of unmixing techniques [e.g., Robertson and France, 1994; Kruiver et al., 2001; Heslop et al., 2002; Egli, 2004].”
- Using time- and temperature-dependent Preisach models to investigate the limitations of modelling isothermal remanent magnetization acquisition curves with cumulative log Gaussian functions (2004, methodology): “Kruiver et al. (2001) proposed that the linear additivity of the different lognormal coercivity components would only hold in the absence of interactions, whereas Heslop et al. (2002) suggested that no interactions should be present if CLG analysis was to be applied successfully.”
- MAX UnMix: A web application for unmixing magnetic coercivity distributions (2016, methodology): “, 2001) or automated iterative approaches (Expectation Algorithm; Heslop et al., 2002).”
- Selected room temperature magnetic parameters as a function of mineralogy, concentration and grain size (2003, background): “1 is rRS=v plotted against the remanent coercivity, ðB0ÞCR, (cf. Thompson and Oldfield, 1986; Peters and Thompson, 1998).”
- Searching for single domain magnetite in the “pseudo‐single‐domain” sedimentary haystack: Implications of biogenic magnetite preservation for sediment magnetism and relative paleointensity determinations (2012, methodology): “Fourth, we use Mr acquisition curve analysis [Robertson and France, 1994; Kruiver et al., 2001; Heslop et al., 2002].”
- Environmental magnetism: Principles and applications (2012, background): “For example, IRM acquisition curves can be decomposed into different coercivity fractions [Robertson and France, 1994; Kruiver et al., 2001; Heslop et al., 2002; Egli, 2004a, 2004b, 2004c].”
- Characterization of Individual Rock Magnetic Components by Analysis of Remanence Curves, 1. Unmixing Natural Sediments (2004, methodology): “Later developments of this method were concerned with the minimization procedure (Stockhausen, 1998; Heslop et al., 2002 ), and the significance of the model, which depends on the number of model functions used (Kruiver et al., 2001).”