Ten-year helium anomaly prior to the 2014 Mt Ontake eruption
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作者:
Sano, Yuji
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Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
Natl Taiwan Univ, Dept Geosci, Taipei 10764, TaiwanUniv Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
Sano, Yuji
[1
,2
]
Kagoshima, Takanori
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Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, JapanUniv Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
Kagoshima, Takanori
[1
]
Takahata, Naoto
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Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, JapanUniv Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
Takahata, Naoto
[1
]
Nishio, Yoshiro
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Kochi Univ, Res & Educ Fac, Nankoku, Kochi, JapanUniv Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
Nishio, Yoshiro
[3
]
Roulleau, Emilie
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Univ Chile, Dept Geol, CEGA, Santiago, ChileUniv Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
Roulleau, Emilie
[4
]
Pinti, Daniele L.
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Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada
Univ Quebec, Dept Sci Terre & Atmosphere, Montreal, PQ H3C 3P8, CanadaUniv Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
Pinti, Daniele L.
[5
,6
]
Fischer, Tobias P.
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Univ New Mexico, Dept Earth & Planetary Sci, Albuquerque, NM 87131 USAUniv Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
Fischer, Tobias P.
[7
]
机构:
[1] Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
Mt Ontake in central Japan suddenly erupted on 27th September 2014, killing 57 people with 6 still missing. It was a hydro-volcanic eruption and new magmatic material was not detected. There were no precursor signals such as seismicity and edifice inflation. It is difficult to predict hydro-volcanic eruptions because they are local phenomena that only affect a limited area surrounding the explosive vent. Here we report a long-term helium anomaly measured in hot springs close to the central cone. Helium-3 is the most sensitive tracer of magmatic volatiles. We have conducted spatial surveys around the volcano at once per few years since November 1981. The He-3/He-4 ratios of the closest site to the cone stayed constant until June 2000 and increased significantly from June 2003 to November 2014, while those of distant sites showed no valuable change. These observations suggest a recent re-activation of Mt Ontake and that helium-3 enhancement may have been a precursor of the 2014 eruption. We show that the eruption was ultimately caused by the increased input of magmatic volatiles over a ten-year period which resulted in the slow pressurization of the volcanic conduit leading to the hydro-volcanic event in September 2014.
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Smithsonian Institution, 2014, SMITHS I WEEKL REP