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- 菊地 正幸
- 東京大学地震研究所
書誌事項
- タイトル別名
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- the 1995 Amami-Oshima-Kinkai (Kikai-jima-Kinkai) Earthquake and Its Tectonics. Rupture Process of the 1995 Amami-Oshima-Kinkai Earthquakes Inferred from Teleseismic Data.
- エンチ ジッタイハ ニヨル 1995ネン アマミ オオシマ キンカイ ジシン
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抄録
Several earthquakes, which occurred near Kikai-jima from October 18 to November 1, 1995, are examined by means of teleseismic body waves. All the focal mechanisms determined for these earthquakes reveal normal-faults having a down-dip extension within a subducting slab. The main source parameters of the largest event are : (strike, dip, rake) = (208°, 75°, -92°); the seismic moment=5.9×1019 [Nm] (Mw=7.1); fault area =6.0×108 [m2];dislocation=1.5 [m]; rupture duration=23 [s]; stress drop =10 [MPa]. In this event the rupture propagated unilaterally to SW direction. The second largest event ruptured the NE region, where the fault plane did not smoothly connected but formed a step to the main fault plane. It may be noteworthy that these earthquakes did not trigger any significant inter-plate earthquakes, suggesting that the adjacent plate interface may be intrinsically aseismic.
収録刊行物
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- 地学雑誌
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地学雑誌 106 (4), 537-545, 1997
公益社団法人 東京地学協会
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詳細情報 詳細情報について
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- CRID
- 1390282679206492672
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- NII論文ID
- 10002236284
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- NII書誌ID
- AN00322536
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- ISSN
- 18840884
- 0022135X
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- NDL書誌ID
- 4283310
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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
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- 抄録ライセンスフラグ
- 使用不可