摘要：Volcanic tremor is often observed to be associated with an increase in volcanic activity and during periods approaching eruptions.It is therefore of crucial importance to study this phenomenon.The opening of a new vent and subsequent ash–gas emissions was observed in the active crater (Nakadake crater) of Aso volcano, Japan, in January 2014.These events were considered to be associated with phreatomagmatic activity similar to the small events of 2003–2005.During the period from December 2013 to January 2014, a significant variation in the amplitude of continuous seismic tremors was observed corresponding to surficial volcanic activity.We estimated the tremor source locations for this two-month period by a three-dimensional grid search using the tremor amplitude ratio of 5–10 Hz band-pass filtered waveforms.The estimated source locations were distributed in a roughly cylindrical region (100–150 m in diameter) ranging from the ground surface to a depth of 400 m.Migration of the estimated source location was also identified and was associated with changes in volcanic activity.We assumed that the source locations coincided with a conduit system of the volcano, consisting of networks of fractures.This area is likely situated above the crack-like conduit proposed in previous studies.Before the 2014 event, an increase in gas-dominated volcanic fluid first caused an enlargement of the conduit zone, followed by the migration of further magmatic fluid through other pathways, which resulted in a subsequent ash–gas emission.Although we do not have sufficient information to discuss the causal relationship between these processes, it seems reasonable that continuous tremors might change the conduit conditions.
