Paleomagnetic direction of the Lower Miocene Hokusetsu Subgroup in the Shitara area, Aichi Prefecture, and implications for the formation of the cuspate geologic structure in central Honshu-Reference-Cited by-同舟云学术

Paleomagnetic direction of the Lower Miocene Hokusetsu Subgroup in the Shitara area, Aichi Prefecture, and implications for the formation of the cuspate geologic structure in central Honshu

Published:2012-11-15 Issue:11 Volume:118 Page:748-761
ISSN:0016-7630
Container-title:The Journal of the Geological Society of Japan
language:en
Short-container-title:Jour. Geol. Soc. Japan

Author:

Hoshi Hiroyuki¹,Ogawa Koichi²

Affiliation:

1. Department of Earth Sciences, Aichi University of Education

2. Graduate, Aichi University of Education

Publisher

The Geological Society of Japan

Subject

General Earth and Planetary Sciences,General Engineering,General Environmental Science

Link

https://www.jstage.jst.go.jp/article/geosoc/118/11/118_2012.0050/_pdf

Reference68 articles.

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2. 青池寛 (Aoike, K.), 1999, 伊豆衝突帯の構造発達．神奈川県博調査研報 (自然) (Res. Rep. Kanagawa Pref. Mus. Nat. Hist.), 9, 111-151.

3. Biggin, A. J., Strik, G. H. M. A. and Langereis, C. G., 2008, Evidence for a very-long-term trend in geomagnetic secular variation. Nature Geosci., 1, 395-398.

4. Brock, A., 1971, An experimental study of palaeosecular variation. Geophys. Jour. Roy. Astron. Soc., 24, 303-317.

5. Cox, A., 1969, Confidence limits for the precision parameter κ. Geophys. Jour. Roy. Astron. Soc., 17, 545-549.

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