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• W2313200832 abstract "Three magnetic components were recognized in the natural remanent magnetization of the Pliocene Takafu Mudstone Member of the Shigarami Formation in the Takafu Syncline in the western part of the North Fossa Magna, central Japan, by means of progressive alternative field and thermal demagnetizations. The first component is attributed to a present-day field overprint or drilling disturbances. The second component, which constitutes the absolute majority of the natural remanent magnetization, is demagnetized at temperatures up to 100-400°C. The third component, which comprises less than 30% of the natural remanent magnetization, is demagnetized at temperatures between 300 and 600°C. The second and third components were detected at 26 sites and at 13 sites, respectively. X-ray diffraction analyses indicated that the Takafu Mudstone contains ferrimagnetic either magnetite or greigite (Fe3S4), or both. A sample in which only the second component was detected, contains greigite only, whereas magnetite is responsible for the third component. Microscopic observations also confirmed formation of authigenic greigite in the Takafu Mudstone. I conclude that the second component is the chemical remanent magnetization (CRM) of greigite, and the third component is the post-depositional remanent magnetization (pDRM) of magnetite. The third component display magnetic direction similar to the second component, and both components passed the fold test (bootstrap method of Tauxe and Watson, 1994). This suggests that both magnetizations were acquired before folding of the Takafu Syncline and that the Takafu Mudstone of pro-fan-delta sediments origin, recorded CRM that is more stable than pDRM within a certain geologic time." @default.
• W2313200832 created "2016-06-24" @default.
• W2313200832 creator A5081051760 @default.
• W2313200832 date "2004-01-01" @default.
• W2313200832 modified "2023-09-27" @default.
• W2313200832 title "Chemical remanent magnetization of the greigite (Fe3S4)-bearing Takafu Mudstone Member in the North Fossa Magna, central Japan" @default.
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• W2313200832 doi "https://doi.org/10.4096/jssj1995.59.1" @default.
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