scholarly journals A block-fault model for deformation of the Japanese Islands derived from continuous GPS observation

2000 ◽  
Vol 52 (11) ◽  
pp. 1095-1100 ◽  
Author(s):  
Manabu Hashimoto ◽  
Shin’ichi Miyazaki ◽  
David D. Jackson
2012 ◽  
Vol 7 (1) ◽  
pp. 26-36 ◽  
Author(s):  
Masato Iguchi ◽  
◽  
Surono ◽  
Takeshi Nishimura ◽  
Muhamad Hendrasto ◽  
...  

We report methods, based on geophysical observations and geological surveys, for the prediction of eruptions and the evaluation of the activity of 4 volcanoes in Indonesia. These are Semeru, Guntur, Kelud and Sinabung volcanoes. Minor increases in tilt were detected by borehole tiltmeters prior to eruptions at the Semeru volcano depending on the seismic amplitude of explosion earthquakes. The results show the possibility of prediction of the type and magnitude of eruption and the effectiveness of observation with a high signalto-noise ratio. The establishment of background data is important for evaluating volcanic activity in longterm prediction. Typical distributions of volcanic and local tectonic earthquakes were obtained around the Guntur volcano, where geodetic monitoring by continuous GPS observation is valuable. The cumulative volume of eruptive products is valuable for evaluating the potential for future eruption. The eruptive rate of the Kelud volcano is ca 2×106m3/y (dense rock equivalent), but the volume of the 2007 eruption was only 2×107m3, suggesting a still high potential for eruption. Based on geological surveys and dating, an eruption scenario is proposed for the activity of Mt. Sinabung, where phreatic eruptions occurred in 2010 after a historically long dormancy.


2015 ◽  
Vol 10 (1) ◽  
pp. 106-112
Author(s):  
Akimichi Takagi ◽  
◽  
Kenji Fujiwara ◽  
Takahiro Ohkura ◽  
Artemio C. Luis ◽  
...  

Determining the location and the amount of volume change of the pressure source beneath a volcano during the eruption preparation stage is an important issue in monitoring the magma accumulation. To do so, we have implemented a GPS campaign survey network around the Mayon volcano and monitored ground deformation since 2005. Rapid grounddeflating deformation was detected accompanied by the 2009 eruption. The Mogi model pressure source was estimated to be 8.5 km deep beneath the summit and the amount of volume change –13 × 106 m3. In magma accumulation preceding the 2009 eruption, ground deformation showed a weak inflationary trend, but it was difficult to evaluate the source parameters definitively. After the 2009 eruption, no deformation has been detected by the Continuous GPS observation network since 2012. Trend of many baselines of continuous and campaign network turned to extension since 2014. Magma may have started accumulating beneath the Mayon volcano.


2006 ◽  
Vol 58 (2) ◽  
pp. 127-139 ◽  
Author(s):  
Manabu Hashimoto ◽  
Nithiwatthn Choosakul ◽  
Michio Hashizume ◽  
Shuzo Takemoto ◽  
Hiroshi Takiguchi ◽  
...  

2019 ◽  
Vol 382 ◽  
pp. 173-183 ◽  
Author(s):  
Kohei Hotta ◽  
Masato Iguchi ◽  
Takahiro Ohkura ◽  
Muhamad Hendrasto ◽  
Hendra Gunawan ◽  
...  

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