The paleomagnetism of single silicate crystals: Recording geomagnetic field strength during mixed polarity intervals, superchrons, and inner core growth

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Understanding fine magnetic particle systems through use of first‐order reversal curve diagrams (2014, methodology): “567 only suitable instrument (e.g., for single crystal measurements [e.g., Tarduno et al., 2006]), but generally, the VSM is a more stable platform from which to make FORC measurements.”
The Magnetic Field of Planet Earth (2010, background): “One interesting strategy has been proposed by Cottrell and Tarduno (1999) (see also Tarduno et al. 2006 for a recent review), which consists in using plagioclase crystals, extracted from igneous rocks that otherwise provide poor paleointensity, but good paleodirection records.”
Detection of noninteracting single domain particles using first‐order reversal curve diagrams (2010, background): “Therefore, rocks and single crystals containing such particles as the predominant magnetic phase are ideal for paleointensity studies [Tarduno et al., 2006].”