Increasing the efficiency of paleointensity analyses by selection of samples using first-order reversal curve diagrams
By C. Carvallo, A. Roberts, R. Leonhardt, C. Laj, C. Kissel, M. Perrin, P. Camps. 2006
72 citations recorded by the source corpus.
Subfields: Electronic, Optical and Magnetic Materials, Geophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/171f98b4dfe0d1fcc39893809d913c6dfef68cdf
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In Electronic, Optical and Magnetic Materials
In Geophysics
In Molecular Biology
Citations in the corpus
- 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, background): “…rocks, which are ultimately the primary source of erosional detritus, contain abundant SD material [e.g., Dunlop, 1972; Heider et al., 1993; Tauxe et al., 1996;Carvallo et al., 2006; Paterson et al., 2010], which makes them an obvious and important source of sedimentary paleomagnetic signals.”
- Detection of noninteracting single domain particles using first‐order reversal curve diagrams (2010, background): “…in the geosciences range from an aid for the preselection of appropriate samples for paleointensity determinations [e.g.,Wehland et al., 2005; Carvallo et al., 2006; Tarduno et al., 2006; Yamazaki, 2008], to the characterization of sediments [Roberts et al., 2006; Rowan and Roberts, 2006]…”
- FORCinel: An improved algorithm for calculating first‐order reversal curve distributions using locally weighted regression smoothing (2008, background): “, 2005], preselect samples for paleointensity studies [Wehland et al., 2005; Carvallo et al., 2006], determine magnetic domain states [Acton et al.”
- Understanding fine magnetic particle systems through use of first‐order reversal curve diagrams (2014, methodology): “…et al., 2001; Heslop et al., 2002; Egli, 2004]; much useful information can be obtained from these profiles [e.g., Muxworthy and Dunlop, 2002; Carvallo et al., 2006a; Rowan and Roberts, 2006; Geiss et al., 2008] and by unmixing or other analyses to understand central ridge signatures [e.g.,…”
- Characterization of hematite (α-Fe2O3), goethite (α-FeOOH), greigite (Fe3S4), and pyrrhotite (Fe7S8) using first-order reversal curve diagrams (2006, methodology): “…states and the extent of magnetostatic interactions in paleomagnetism [e.g., Weaver et al., 2002; Rowan and Roberts, 2006; Tarduno et al., 2006; Carvallo et al., 2006a], environmental magnetism [e.g., van Oorschot et al., 2002; Peck et al., 2004; Muxworthy et al., 2005] and rock magnetism…”