1995年奄美大島近海(喜界島近海)地震の地震活動とテクトニクス 遠地実体波による1995年奄美大島近海地震の震源過程

書誌事項

タイトル別名
  • 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

  • 地学雑誌

    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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