[S-VC12] Multidisciplinary volcano monitoring

[SVC12-P06] インドネシアLUSI泥火山噴火にともなう地殻変動

*青木 陽介¹、Sidiq Teguh Purnama² (1.東京大学地震研究所、2.バンドン工科大学)

キーワード：泥火山, 地殻変動, 合成開口レーダー, 時系列解析

Ground deformation associated with the eruption of Lumpur Sidoarjo mud volcano between 2006 and 2011 has been investigated from Synthetic Aperture Radar images. Marked subsidence has been observed to the west of, as well as around, the vent. Line-of-sight changes in the both areas decayed since the middle of 2008 with a time constant of 1.5?2.5 years, implying that the ongoing eruption won't last long. This uniform decay time indicates that the western part is connected to the eruption center since the middle of 2008 to form a system with station- ary geometry. Our observation that the decay started later to the west than around the vent suggests that the sub- sidence to the west has been triggered by the mud eruption. A simple modeling suggests that 1) the conduit needs to be narrower at depth than at the surface, 2) the effective rigidity of the mud needs to be lower than that estimated from the drilled sample, or both to explain the observed decay constant of the deformation.