Global positioning system measurements of ground deformation caused by magma intrusion and lava discharge: the 1990-1995 eruption at Unzendake volcano, Kyushu, Japan
K. Nishi et al., Global positioning system measurements of ground deformation caused by magma intrusion and lava discharge: the 1990-1995 eruption at Unzendake volcano, Kyushu, Japan, J VOLCANOL, 89(1-4), 1999, pp. 23-34
Global positioning system (GPS) measurements made around Unzendake volcano,
Kyushu, Japan, since January 1991 have detected ground deformation caused
by magma intrusion and lava discharge. In the intermittent phreatic and phr
eatomagmatic eruption stage, the ground was inflating. After growth of the
lava dome and following frequent pyroclastic flows at Unzendake volcano, th
e ground began deflating. These ground deformations are explained by the in
flation and deflation of a Mogi's source model (a point source model) locat
ed about 6 km west of the active crater at a depth of 11 km, at an aseismic
region. The observed horizontal displacement vectors pointed radially away
from the estimated pressure source during inflation and pointed to the pre
ssure source during deflation. The horizontal displacements at the referenc
e GPS station calculated from contraction of the estimated pressure source
coincide well with the actual horizontal displacements observed from other
GPS baseline systems. These observations validate our estimates for the pre
ssure source. Based on the relation between the deformation volume of the g
round surface and the discharged volume of the lava, it is estimated that d
uring the eruption there was magma supply from the deeper portion as well a
s magma discharge at the crater. Magma is estimated to be supplied to the r
eservoir at an average rate of 1.1x10(5) m(3)/day; magma intrusion began in
December 1989 at the latest and continued for 1.9 x 10(3) days. (C) 1999 E
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