Transient crustal deformation is often observed in conjunction with earthquake swarms and is attributed to aseismic processes that drive swarm activity, such as magma intrusion, fluid migration, or slow slip events. Off the Tokara Islands, along the volcanic front of the Ryukyu subduction zone in the southern Japanese Archipelago, earthquake swarms have repeatedly occurred; however, the driving mechanism of this anomalous seismicity remains unclear. Here, we investigate this mechanism through integrative analyses of Global Navigation Satellite Systems (GNSS) data from the Geospatial Information Authority of Japan and SoftBank Corp. The daily GNSS position time series at multiple stations exhibits clear transient signals that coincide with recurrent earthquake swarms. Notably, during the June–July 2025 episode, both the temporal trend and spatial pattern of the displacement changed abruptly at the onset of the secondary swarm. Motivated by these distinctive characteristics, we estimated the source models for the 2025 episode by dividing it into three phases. For all phases, the displacements calculated from rectangular faults with shear slip reproduce the observed displacements well. Vertical open cracks provide an alternative source model, but their data fit is systematically worse than that of the shear-slip models. A stacked time series of 30-s kinematic GNSS positions further suggests that the temporal relationship between aseismic deformation and seismicity can vary even within a single episode. Based on the shear-slip and open crack models for the 2025 episode, we propose two scenarios for the driving mechanisms of aseismic displacements and earthquake swarms. In both scenarios, we speculate that the supply of material from a region deeper than the aseismic source and swarm hypocenters plays a key role in generating these episodes.
Okada et al. (Wed,) studied this question.