Spatio-temporal characteristics and focal mechanisms of deep low-frequency earthquakes beneath the Zao volcano, northeastern Japan
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DOI: 10.1016/j.jvolgeores.2021.107321
Abstract: Abstract Deep low-frequency earthquakes (DLFs) beneath volcanoes are possible evidence for deep-seated magmatic activity in the mid-to-lower crust and uppermost mantle. After the 2011 Tohoku-oki earthquake (Mw 9.0), the number of DLFs beneath the Zao… read more here.
Keywords: deep low; zao volcano; low frequency; focal mechanisms ... See more keywords