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- W2107007188 abstract "Fifty-four palaeointensity values, measured by the Thellier technique, are used to study the cause of reversal asymmetry in late Precambrian Keweenawan rocks. These data, obtained mainly from diabase dykes carrying primary TRM and their baked host rocks, show that ‘reversed’ palaeointensities are on average 40 per cent higher than their ‘normal’ counterparts. This result cannot be explained by any overall difference in remanence characteristics, grain size or cooling rate (dyke width) between the rocks comprising the two polarity groups. A significant difference in the local intensity of the geomagnetic field between times of normal and reversed polarity is thus indicated. This conclusion is reinforced by positive baked contact tests for both normal and reversed Thellier palaeointensities." @default.
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- W2107007188 date "1983-04-01" @default.
- W2107007188 modified "2023-10-16" @default.
- W2107007188 title "Geomagnetic field intensity and reversal asymmetry in late Precambrian Keweenawan rocks" @default.
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- W2107007188 doi "https://doi.org/10.1111/j.1365-246x.1983.tb03816.x" @default.
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