Journal of Disaster Research
Online ISSN : 1883-8030
Print ISSN : 1881-2473
ISSN-L : 1881-2473
Special Issue on NIED Frontier Research on Science and Technology for Disaster Risk Reduction and Resilience 2020
Subsurface Resistivity Imaging of Nasudake (Chausudake) Volcano Determined from Time Domain Electromagnetic Survey (TDEM)
Toshikazu TanadaYoichi Nakamura
著者情報
ジャーナル 認証あり

2020 年 15 巻 6 号 p. 735-744

詳細
抄録

A time domain electromagnetic survey (TDEM method) was conducted to investigate the resistivity structure of the crater, fumarole, and hot spring area of the Nasudake (Chausudake) volcano. The findings of this survey are as follows: (1) Under the crater area, a thin low-resistivity layer (approximately 50 m) was found on the surface, and lens-shaped high-resistivity areas continued to a depth of 800 m below it. The lens-shaped high-resistivity areas are believed to correspond to a thermal volcanic gas region. (2) From the east-west direction survey line crossing the foot of the Nasudake, two or three horizontal resistivity layer structures, which are considered to be caused by the geological structure and surface water, were observed.

著者関連情報

この記事は最新の被引用情報を取得できません。

© 2020 Fuji Technology Press Ltd.
前の記事 次の記事
feedback
Top