Project Details
Abstract
Thus, the possibility is strengthened that the aseismic part of the relative plate motion in the south of the Sanriku region is released episodically with various time constants such as the ultra-slow earthquake.
Status | Finished |
---|---|
Effective start/end date | 1992/01/01 → 1993/12/31 |
Funding
- Japan Society for the Promotion of Science: ¥1,600,000.00
Keywords
- スロー・ア-スクエイク
- 地殻変動連続観測
- 歪ステップ
- 津波地震
- 1992年三陸沖地震
- 時定数
- ベイズ法
- BAYTAP-G
- スロー・アースクエイク
- スローアースクエイク
- 日本海溝
- BATAP-G
- 地殻歪
- 1992年岩手県沖地震
- slow earthquake
- extensometer
- strain step
- time constant
- 1992 Sanriku earthquake
- tsunami Earthquake
- Bayseian model