摘要:On 27 September 2014, Ontake volcano, in central Japan, suddenly erupted without precursory activity.We estimated and tracked the source locations of volcanic tremor associated with the eruption at high temporal resolution, using a method based on the spatial distribution of tremor amplitudes.Although the tremor source locations were not well constrained in depth, their epicenters were well located beneath the erupted crater and the summit.Tremor sources were seen to descend approximately 2 km over a period of several minutes prior to the beginning of the eruption.Detailed analysis of the time series of tremor amplitudes suggests that this descent is a robust feature.Our finding may be an important constraint for modeling the 2014 eruption of Ontake volcano as well as for monitoring activities on this and other volcanoes.