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

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

Abstract An electrical resistivity model beneath Azumayama Volcano, NE Japan, is explored using magnetotelluric method to probe the magma/hydrothermal fluid distribution. Azumayama is one of the most concerning active volcanoes capable of producing a potential eruption triggered by the 2011 Tohoku-O...

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Bibliographic Details
Main Authors: Masahiro Ichiki, Toshiki Kaida, Takashi Nakayama, Satoshi Miura, Mare Yamamoto, Yuichi Morita, Makoto Uyeshima
Format: Article
Language:English
Published: SpringerOpen 2021-07-01
Series:Earth, Planets and Space
Subjects:
Magnetotellurics
Electrical resistivity
Shear wave velocity
Magma reservoir
Melt fraction
Permeability
Online Access:https://doi.org/10.1186/s40623-021-01451-y

Internet

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

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