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タイトル
  • Magnetotelluric and temperature monitoring after the 2011 sub-Plinian eruptions of Shinmoe-dake volcano
作成者

Aizawa, Koki

Koyama, Takao

Uyeshima, Makoto

Hase, Hideaki

Hashimoto, Takeshi

Kanda, Wataru

Yoshimura, Ryokei

Utsugi, Mitsuru

Ogawa, Yasuo

Yamazaki, Ken'ichi

権利情報
主題
  • Other Magnetotellurics
  • Other temperature monitoring
  • Other resistivity monitoring
  • Other structural change
  • NDC 453
内容注記
Other
  • Three sub-Plinian eruptions took place on 26–27 January 2011 at Shinmoe-dake volcano in the Kirishima volcanic group, Japan. During this event, GPS and tiltmeters detected syn-eruptive ground subsidence approximately 7 km to the WNW of the volcano. Starting in March 2011, we conducted broad-band magnetotelluric (MT) measurements at a site located 5 km NNW of the volcano, beneath which the Shinmoe-dake magma plumbing system may exist. In addition, temperature monitoring of fumaroles and hot-springs near the MT site was initiated in July 2011. Our MT data record changes in apparent resistivity of approximately ±5%, along with a ±1◦ phase change in the off-diagonal component of the impedance tensor (Zxy and Zyx ). Using 1-D inversion, we infer that these slight changes in resistivity took place at relatively shallow depths of only a few hundred meters, at the transition between a near-surface resistive layer and an underlying conductive layer. Resistivity changes observed since March 2012 are correlated with the observed temperature increases around the MT monitoring site. These observations suggest the existence beneath the MT site of pathways which enable volatile escape.
日付 Issued 2013
言語eng
資源タイプjournal article
出版タイプVoR
資源識別子 URI http://hdl.handle.net/2115/67562
関連
  • isIdenticalTo DOI https://doi.org/10.5047/eps.2013.05.008
収録誌情報
    • ISSN 1343-8832
    • ISSN 1880-5981
    • Earth, Planets and Space
    65(6), 539-550
ファイル
コンテンツ更新日時2019-10-09T04:24:05Z