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- W2034585904 abstract "[1] To better understand the fundamentals of Thellier-type absolute geomagnetic field intensity determinations, a map of χ was constructed from the experimental blocking versus unblocking relation. Once constructed, the map of χ can predict the outcome of a Thellier experiment. Thellier predictions were compared with an independent Thellier experiment. The contribution from low- and high-temperature partial thermoremanent magnetization (pTRM) tails increased as the grain size of magnetite increased, indicating a progressive violation of pTRM reciprocity in the multidomain (MD) range. Such a violation of reciprocity with increasing grain size generated enhancement of down-sagging features in Arai plots, a primary reason for the failure of Thellier experiments. As anticipated, MD magnetites displayed broad unblocking spectra, while single-domain grains showed a narrow inflection. Overall, the mapping of χ was useful in predicting key features in the Thellier experiment. However, as the grain size increased, there was a growing discrepancy between prediction and experiments, possibly caused by the initial state dependence of pTRM intensity." @default.
- W2034585904 created "2016-06-24" @default.
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- W2034585904 date "2009-04-01" @default.
- W2034585904 modified "2023-09-23" @default.
- W2034585904 title "Properties of partial thermoremanence in magnetite: Testing the blocking versus unblocking temperature spectrum using the phenomenological model" @default.
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- W2034585904 doi "https://doi.org/10.1029/2008jb006065" @default.
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