Long-term variations in palaeointensity

By P. Selkin, Lisa Tauxe. Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 2000

372 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geophysics, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/e71a880341dd6e23171502be620af7483b63ac32

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Citations in the corpus

The Magnetic Field of Planet Earth (2010, background): “Some authors (e.g. Juarez et al. 1998; Selkin and Tauxe 2000; Juarez and Tauxe 2000), relying on submarine basaltic glasses, have argued that significantly higher values are found only when considering data younger than 300 ky. [This, incidentally, is the reason why Tauxe and Kent (2004) chose a…”
The application of acceptance criteria to results of Thellier palaeointensity experiments performed on samples with pseudo-single-domain-like characteristics (2003, methodology): “Difficulties associated primarily with thermo-chemical alteration of samples in the laboratory have led to the introduction of a series of acceptance criteria which must be fulfilled in order that a palaeointensity estimate may be regarded as reliable (e.g.Coe et al., 1978; Selkin and Tauxe, 2000).”
The intensity of the geomagnetic field in the late-Archaean: new measurements and an analysis of the updated IAGA palaeointensity database (2009, methodology): “The KolmogorovSmirnov test (KS test, Selkin and Tauxe, 2000) was used to provide a test for the two datasets having been drawn from statistically-distinct distributions.”
Thermal and magnetic evolution of the Earth’s core (2003, background): “Such a change is rather small compared to the variations observed in the intensity of the dipole in the last 300 Ma(Selkin and Tauxe, 2000; Labrosse and Macouin, 2003)which, obviously, cannot all be attributed to the appearance of the inner core.”
The paleomagnetism of single silicate crystals: Recording geomagnetic field strength during mixed polarity intervals, superchrons, and inner core growth (2006, background): “This work supersedes prior studies using this material [e.g., Pick and Tauxe, 1993; Selkin and Tauxe, 2000], which RG1002 Tarduno et al.: PALEOMAGNETISM OF SINGLE SILICATE CRYSTALS 10 of 31 RG1002 concluded that the Superchron field was weak or of average strength.”
Energetics of the Core (2015, background): “The magnetic field intensity has fluctuated over time, with the present-day magnetic field being anomalously strong (Selkin and Tauxe 2000), and the field during the Mesozoic anomalously weak (Prevot et al. 1990).”
Analyzing absolute paleointensity determinations: Acceptance criteria and the software ThellierTool4.0 (2004, methodology): “Allowing only a 25% variation of the paleointensity values [Selkin and Tauxe, 2000] within a cooling unit creates problems when dealing with low intensities.”
Source of oceanic magnetic anomalies and the geomagnetic polarity time scale (2007, background): “For example, the NRM of the near-axis samples may be biased by high paleointensities over the past few thousand years that were up to a factor of 2 higher than today’s field and perhaps a factor of 4 higher than the average long-term paleofield intensity (Selkin and Tauxe, 2000).”