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Magma reservoir beneath Azumayama Volcano, NE Japan, as inferred from a three-dimensional electrical resistivity model explored by means of magnetotelluric method

Crossref DOI link: https://doi.org/10.1186/s40623-021-01451-y

Published Online: 2021-07-27

Published Print: 2021-12

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Ichiki, Masahiro https://orcid.org/0000-0003-0814-1265
Kaida, Toshiki

Nakayama, Takashi

Miura, Satoshi

Yamamoto, Mare

Morita, Yuichi

Uyeshima, Makoto
Funding

Funding for this research was provided by:

Ministry of Education, Culture, Sports, Science and Technology (Program of Mobile and Intensive Observation-Research System Integration for Volcanic Areas)

Ministry of Education, Culture, Sports, Science and Technology (Earthquake and Volcano Hazards Observation and Research Program, Earthquake and Volcano Hazards Observation and Research Program, Earthquake and Volcano Hazards Observation and Research Program)
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Text and Data Mining valid from 2021-07-27

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Article History

Received: 29 December 2020

Accepted: 5 June 2021

First Online: 27 July 2021

Declarations

:

: Not applicable.

: Not applicable.

: The authors have no competing interests.

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