書誌事項
- タイトル別名
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- 14C Ages and Geomagnetic Reversals of the Shibutami Welded Tuff Bed in the Northern Part of Morioka
- モリオカ ホクブ ノ シブタミ ヨウケツ ギョウカイガンソウ アクセキ ノ 1
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The Shibutami welded tuff bed characterized by the geomagnetic reversals is distributed along the Kitakami river between Numakunai (141°15'E , 40°N) and Morioka ( 141° 10'E, 39°40'N), and it is estimated to have been erupted as the nuee ardente from Hachimantai volcano which is located at the western side of this area. The 14C ages were measured on the two samples obtained from the Shitozawa sand and gravel ted intercalated with the welded tuff bed at Shimoda (Shibutami) in the northern part of Morioka. The 14C ages are shown as follows. Sample no. 1 30,780 ± 2170 yr BP (Gak-6356) Sample no. 2 29,630 + 2130 yr BP (Gak-6794) Accordingly the geomagnetic reversals of the Shibutami welded tuff bed (about 30,000 ± yr BP) may be related to the Laschamp event (20,000-30,000 yr BP) in the Brunhes Normal Epoch (Bonhommet, N. and Zahringer, J., 1969 and Cox, A., 1969) and to the geomagnetic excursion 30,000 yr BP (Barbetti, M. and McElhinny, M., 1972).
収録刊行物
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- 岩手大学教育学部研究年報 = Annual report of the Faculty of Education, University of Iwate
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岩手大学教育学部研究年報 = Annual report of the Faculty of Education, University of Iwate 37 159-175, 1977-11-30
岩手大学教育学部
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詳細情報 詳細情報について
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- CRID
- 1390009224895753472
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- NII論文ID
- 120001124041
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- NII書誌ID
- AN00017940
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- ISSN
- 03677370
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- NDL書誌ID
- 1914976
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- IRDB
- NDL
- CiNii Articles