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Detailed Reference Information |
Mankinen, E.A. and Champion, D.E. (1993). Broad trends in geomagnetic paleointensity on Hawaii during holocene time. Journal of Geophysical Research 98: doi: 10.1029/93JB00024. issn: 0148-0227. |
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Paleointensity determinations have been obtained from 22 basaltic lava flows on the island of Hawaii using the Thelliers' method. Radiocarbon dating indicates that these flows erupted at intervals ranging from about 200 to 1000 years, and results of the experiments provide an estimate of broad trends in geomagnetic paleointensity during Holocene time in the vicinity of Hawaii. Most of the samples were obtained from quickly cooled flow margins and, as a consequence, typically contain two titanomagnetite populations. Only two of the 79 samples analyzed failed to yield an estimate of the paleofield, demonstrating that paleointensities can be obtained from such samples if carefully selected. Virtual dipole moments calculated for the flows are compared with a published curve of dipole field intensity that was constructed using worldwide archeomagnetic data. The large nondipole fields that were previously postulated for the vicinity of Hawaii are confirmed, and the present data indicate that they were present from about 5000 years B.P. to perhaps as recently as the past 200 years. The data indicate, however, that these nondipole sources must have been virtually absent between about 12,000 and 5000 years B.P. as they are at the present time. |
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Abstract |
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Table 1 |
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Table 2A |
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Table 2B |
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Table 3A |
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Keywords
Geomagnetism and Paleomagnetism, Time variations—secular and long term, Geomagnetism and Paleomagnetism, Instruments and techniques, Information Related to Geographic Region, Pacific Ocean, Information Related to Geologic Time, Cenozoic |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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