書誌事項
- タイトル別名
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- Isostasy Over Central Honshu, Japan
- ホンシュウ チュウブ チイキ ノ アイソスタシー
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説明
Isostasy over central Honshu area is examined by the following four methods.<br>(1) Cross-spectrum technique is applied to analyse a correlation between Bouguer anomalies and topographic relief over the area. Admittance functions derived from this technique for the area show good agreement with those for stable continents.<br>(2) Residual Bouguer anomalies (R. B. A.) over the area are calculated by subtracting a gravity effect of the subducting Philippine sea plate from the observed Bouguer anomalies. The relationship between the R. B. A. and topographic releaf shows a higher correlation than that between the observed Bouguer anomalies and topographic relief.<br>(3) Theoretical Bouguer anomalies calculated by using the admittance functions in central Honshu and topographic relief in stable continents are in good agreement with the R. B. A. over the area.<br>(4) Hydrostatic pressure at the Moho along the Atsumi-Noto explosion seismological observation line satisfies the empilical rule between depth of Moho and pressure at it, which was found in tectonically stable continental and oceanic areas.<br>It is shown from these results that the isostatic state is achieved over central Honshu as it does over stable continents, though the area is tectonically quite active.
収録刊行物
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- 地震 第2輯
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地震 第2輯 37 (4), 569-578, 1984
公益社団法人 日本地震学会
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詳細情報 詳細情報について
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- CRID
- 1390282679279816832
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- NII論文ID
- 130006783459
- 40001526308
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- NII書誌ID
- AN00305741
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- ISSN
- 18839029
- 2186599X
- 00371114
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- NDL書誌ID
- 3028263
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- データソース種別
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- JaLC
- NDL
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