Two independent signals detected by ocean bottom electromagnetometers during a non-eruptive volcanic event: Ogasawara Island arc volcano, Nishinoshima

Two independent signals detected by ocean bottom electromagnetometers during a non-eruptive volcanic event: Ogasawara Island arc volcano, Nishinoshima

Abstract Nishinoshima is an active oceanic island arc volcano situated approximately 1000 km south of Tokyo, Japan. Since 2016, marine electromagnetic observations using ocean bottom electromagnetometers have been conducted around the island to investigate the electrical structure beneath the volcan...

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Bibliographic Details
Main Authors: Kiyoshi Baba, Noriko Tada, Hiroshi Ichihara, Yozo Hamano, Hiroko Sugioka, Takao Koyama, Akimichi Takagi, Minoru Takeo
Format: Article
Language:English
Published: SpringerOpen 2020-08-01
Series:Earth, Planets and Space
Subjects:
Nishinoshima
Oceanic island arc volcano
Ocean bottom electromagnetometer
Total magnetic force
Volcanic edifice deformation
Online Access:http://link.springer.com/article/10.1186/s40623-020-01240-z

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http://link.springer.com/article/10.1186/s40623-020-01240-z

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