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Seismic campaign in Showa-
Shinzan lava dome in Usu
Volcano, Northern Japan
1 October, 2019
ISTerre, France
A. Takeo1, K. Nishida1, Y. Aoki1, H. Aoyama2, M. Ishise1,
T. Maeda3, Y. Mizutani1, T. Kai1, Y. Nakashima1, S. Nagahara1,
R. Kurihara1, L. Ye4, X. Wang5, T. Akuhara1
1ERI, Univ. Tokyo, 2Hokkaido Univ., 3Hirosaki Univ.
4Sun Yat-sen Univ., 5Southwest Jiaotong Univ.
Internal structure of lava domes
Goto & McPhie (JVGR, 1998)
In-situ observation of exposures can view only the shallowest
part of the intruded lava.
Usu Volcano and Showa-Shinzan lava dome
1910
Activity time
Eruptive
Interval (yr)
Location Eruption type
Upheaval
height (m)
July ̶ Nov. 1910 57 North flank Phreatic 170
Dec. 1943 ̶ Sep.
1945
33 East flank Phreatomagmatic 280
Aug. 1977 ̶ Mar.
1982
32 Summit Phreatomagmatic 180
Mar. ̶ Aug. 2000 18 West flank Phreatomagmatic 80
A phreatomagmatic eruption in 2000
Showa Shinzan that emerged during
the 1943-1945 eruption
280 m
Muon radiography + Gravity
1910
図2. 三松ダイ アグラ ムと
隆起中の火口写真(三松2004; 加筆)
山頂
図4. 密度構造(Nishiyama et al. 2017より )
 High density at the core of
the lava dome.
 Seismic velocity combined
with density gives elastic
constants, thus material
properties.
Seismic campaign
1910
 22 1-Hz seismometers
(7 on the summit, 10
on the flank, and 5 on
the foot)
 Instrumental response
pre-calibrated.
 Recorded ambient
noise to infer the
velocity structure
て暫定1次元速度構造を推定し た。
の順にS波速度が速いこ と がわかっ た。
CCs and phase
velocities:
Summit
1910
4Hz
2Hz
1Hz
山頂付近 屋根山
CCs and phase
velocities: flank
1910 4Hz
2Hz
1Hz
屋根山
CCs and phase
velocities: foot
1910
山頂付近
麓
屋根山
図12. (左)3グループそれぞ
(右)標高をずら し た
4Hz
2Hz
1Hz
麓
Phase and S-wave velocities
1910
Red: Summit
Green: Flank
Blue: Foot
Some earthquake signals
1910
付近の地中で発生し たと 見ら れる低周波地震の波形も 得るこ と ができ
まと め・ 今後の展望
図13. 2018/ 5/ 12 21:03:00から 1分間の波形
( 花火)
図14. 2018/ 6/ 3 00:01:00から 1分間の波形
( 山頂から 順に並べた; 山頂付近の低周波地震?)
近の地中で発生し たと 見ら れる低周波地震の波形も 得るこ と ができ た
と め・ 今後の展望
図13. 2018/ 5/ 12 21:03:00から 1分間の波形
( 花火)
図14. 2018/ 6/ 3 00:01:00から 1分間の波形
( 山頂から 順に並べた; 山頂付近の低周波地震?)
1 min. 1 min.
Firework Low-frequency earthquake
near the summit
Near the summit
Far from the summit

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2019-10-01 Seismic campaign in Showa-Shinzan lava dome in Usu Volcano, Northern Japan

  • 1. Seismic campaign in Showa- Shinzan lava dome in Usu Volcano, Northern Japan 1 October, 2019 ISTerre, France A. Takeo1, K. Nishida1, Y. Aoki1, H. Aoyama2, M. Ishise1, T. Maeda3, Y. Mizutani1, T. Kai1, Y. Nakashima1, S. Nagahara1, R. Kurihara1, L. Ye4, X. Wang5, T. Akuhara1 1ERI, Univ. Tokyo, 2Hokkaido Univ., 3Hirosaki Univ. 4Sun Yat-sen Univ., 5Southwest Jiaotong Univ.
  • 2. Internal structure of lava domes Goto & McPhie (JVGR, 1998) In-situ observation of exposures can view only the shallowest part of the intruded lava.
  • 3. Usu Volcano and Showa-Shinzan lava dome 1910 Activity time Eruptive Interval (yr) Location Eruption type Upheaval height (m) July ̶ Nov. 1910 57 North flank Phreatic 170 Dec. 1943 ̶ Sep. 1945 33 East flank Phreatomagmatic 280 Aug. 1977 ̶ Mar. 1982 32 Summit Phreatomagmatic 180 Mar. ̶ Aug. 2000 18 West flank Phreatomagmatic 80
  • 4. A phreatomagmatic eruption in 2000 Showa Shinzan that emerged during the 1943-1945 eruption 280 m
  • 5. Muon radiography + Gravity 1910 図2. 三松ダイ アグラ ムと 隆起中の火口写真(三松2004; 加筆) 山頂 図4. 密度構造(Nishiyama et al. 2017より )  High density at the core of the lava dome.  Seismic velocity combined with density gives elastic constants, thus material properties.
  • 6. Seismic campaign 1910  22 1-Hz seismometers (7 on the summit, 10 on the flank, and 5 on the foot)  Instrumental response pre-calibrated.  Recorded ambient noise to infer the velocity structure て暫定1次元速度構造を推定し た。 の順にS波速度が速いこ と がわかっ た。
  • 8. CCs and phase velocities: flank 1910 4Hz 2Hz 1Hz 屋根山
  • 9. CCs and phase velocities: foot 1910 山頂付近 麓 屋根山 図12. (左)3グループそれぞ (右)標高をずら し た 4Hz 2Hz 1Hz 麓
  • 10. Phase and S-wave velocities 1910 Red: Summit Green: Flank Blue: Foot
  • 11. Some earthquake signals 1910 付近の地中で発生し たと 見ら れる低周波地震の波形も 得るこ と ができ まと め・ 今後の展望 図13. 2018/ 5/ 12 21:03:00から 1分間の波形 ( 花火) 図14. 2018/ 6/ 3 00:01:00から 1分間の波形 ( 山頂から 順に並べた; 山頂付近の低周波地震?) 近の地中で発生し たと 見ら れる低周波地震の波形も 得るこ と ができ た と め・ 今後の展望 図13. 2018/ 5/ 12 21:03:00から 1分間の波形 ( 花火) 図14. 2018/ 6/ 3 00:01:00から 1分間の波形 ( 山頂から 順に並べた; 山頂付近の低周波地震?) 1 min. 1 min. Firework Low-frequency earthquake near the summit Near the summit Far from the summit