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- W2079163664 abstract "The paleomagnetic field intensity is estimated with the aid of the Koenigsberger-Thellier method for four ordinary chondrites and one carbonaceous chondrite by assuming that the stable NRM component of these meteorites is attributable to the TRM acquired in a low-temperature range (lower than about 400°C) during their extremely-slow cooling process. The results are summarized in Table IV, where the paleomagnetic field intensity ranges from 0.10 to 0.97 Oe. Possible effects of the extremely-slow cooling rate of meteorites and the secondary TRM acquisition of the surface fusion crust upon the original NRM of the meteorite interior are discussed." @default.
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- W2079163664 date "1977-01-01" @default.
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- W2079163664 title "Paleomagnetic field intensity derived from meteorite magnetization" @default.
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- W2079163664 doi "https://doi.org/10.1016/0031-9201(77)90126-1" @default.
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