書誌事項
- タイトル別名
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- Origin of ground water in the Takisaka landslide area, Fukushima Prefecture, estimated from the isotopic properties
- ドウイタイ カラ ミタ フクシマケン タキサカ ヂスベリチ ニ オケル チカスイ ノ キゲン
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説明
This report deals with isotopic properties of ground waters and rocks sampled from the Takisaka landslide area, Fukushima Prefecture. Tritium concentrations of ground waters are the same as that of modern precipitation . Strontium isotope ratios of waters and whole rock samples indicate that ground water in the northern blocks should originate in granite . Oxygen isotope ratio of drainage water in the Numata block is apart from values of the Aga River water and ground water in other blocks . Further investigation and counterpart for ground waters in the northern blocks are required because the movement of these waters is supposed to be derived from peripheral granite zone.
収録刊行物
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- 地すべり
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地すべり 39 (3), 319-325, 2002
公益社団法人 日本地すべり学会
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キーワード
詳細情報 詳細情報について
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- CRID
- 1390001204545062656
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- NII論文ID
- 10011717149
- 10010212482
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- NII書誌ID
- AN00332562
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- ISSN
- 18843956
- 02852926
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- NDL書誌ID
- 6417718
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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
