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Further application of the deconvolution method of post-depositional DRM to the precise record of the Matuyama-Brunhes reversal in the sediments from the Boso Peninsula, Japan

Earth, Planets and Space volume 51, pages 169–173 (1999)Cite this article

Abstract

The Matuyama-Brunhes geomagnetic reversal was continuously recorded in the massive siltstones of the Boso marine sediments in Japan with the time resolution better than 9 years. However the Boso sediments probably have the post-depositional detrital remanent magnetization (pDRM) depressing short-period variations due to the convolution of the geomagnetic field. The previous application of the deconvolution method of pDRM to the 900 year records gave the half fixing depth of 21 cm. Further application of this fixing depth to the 4100 year record clearly shows nearly 100 year variations in both of the inclination and declination.

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Authors and Affiliations

  1. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Tokyo, 152-8551, Japan

    Hideo Tsunakawa

  2. Department of Earth Sciences, Ibaraki University, Mito, Ibaraki, 310-8512, Japan

    Makoto Okada

  3. Department of Geosciences, Shizuoka University, Shizuoka, 422-8529, Japan

    Nobuaki Niitsuma

Authors
  1. Hideo Tsunakawa
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  2. Makoto Okada
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  3. Nobuaki Niitsuma
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Correspondence to Hideo Tsunakawa.

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Tsunakawa, H., Okada, M. & Niitsuma, N. Further application of the deconvolution method of post-depositional DRM to the precise record of the Matuyama-Brunhes reversal in the sediments from the Boso Peninsula, Japan. Earth Planet Sp 51, 169–173 (1999). https://doi.org/10.1186/BF03352221

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  • DOI: https://doi.org/10.1186/BF03352221

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