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• W2072313455 endingPage "249" @default.
• W2072313455 startingPage "237" @default.
• W2072313455 abstract "A new and larger database is established to assess the variation of paleointensity with time. It is shown that submarine basaltic glass probably contains a grain-growth chemical remanent magnetization in magnetite. Intensity estimates from these samples are used to establish a lower bound estimate on intensities. Statistical tests on various subsets of the database are used to establish a more reliable database for finding long-term trends of the paleointensity. We can obtain a reasonable estimate for intensity versus time for the Cenozoic but not for the Mesozoic or late Paleozoic. The distributions of data as a function of time also provide valuable information. In particular, the two well-documented superchrons exhibit different intensity properties, which suggests that there is not a simple correlation between reversal rate and intensity." @default.
• W2072313455 created "2016-06-24" @default.
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• W2072313455 date "2002-08-01" @default.
• W2072313455 modified "2023-10-08" @default.
• W2072313455 title "The variation of intensity of earth’s magnetic field with time" @default.
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• W2072313455 doi "https://doi.org/10.1016/s0031-9201(02)00038-9" @default.
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