書誌事項
- タイトル別名
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- Newly Found Kentoyama Fault in the Northern Part of the Eastern Marginal Area of Fukui Plain, and Its Implications.
- フクイ ヘイヤ トウエン サイホクブ ニ オケル ケントウヤマ ダンソウ ノ ハッケン ト ソノ イギ
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The newly found Kentoyama fault runs through the northeastern part of Fukui plain, and its trend is nearly N-S. Based on the observation of its fault outcrop, Kentoyama fault is composed of a set of three faults, and it deforms marine terrace deposits and sand dune deposits. The strike and dip of the fault surface are N7°-15°and 62°E-90°, respectively.<br>The vertical slip rate of the Kentoyama fault is at least 0.04-0.12m/ky. We cannot estimate the fault scarp on the terrace surface, due to the thick sand dune deposits.<br>As the trend of the Kentoyama fault, which extends N-S direction, corresponds with that of the eastern marginal faults of the Fukui plain, the fault is considered to be an extension of the eastern marginal faults of the Fukui plain.
収録刊行物
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- 第四紀研究
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第四紀研究 40 (1), 67-74, 2001
日本第四紀学会
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詳細情報 詳細情報について
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- CRID
- 1390001206496163840
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- NII論文ID
- 10007543055
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- NII書誌ID
- AN0034136X
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- ISSN
- 18818129
- 04182642
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- NDL書誌ID
- 5655149
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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
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可