Global positioning system measurements of ground deformation caused by magma intrusion and lava discharge: the 1990-1995 eruption at Unzendake volcano, Kyushu, Japan

被引:35
|
作者
Nishi, K
Ono, H
Mori, H
机构
[1] Kyoto Univ, Sakurajima Volcano Res Ctr, DPRI, Kagoshima 8911419, Japan
[2] Kyoto Univ, Fac Sci, Aso Volcanol Lab, Kumamoto 8691400, Japan
[3] Hokkaido Univ, Fac Sci, Usu Volcano Observ, Sohbetsu, Hokkaido 0520103, Japan
关键词
GPS measurement; magma reservoir; supply and discharge rate of magma; ground deformation; Mogi's model;
D O I
10.1016/S0377-0273(98)00119-X
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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 phreatomagmatic eruption stage, the ground was inflating. After growth of the lava dome and following frequent pyroclastic flows at Unzendake volcano, the ground began deflating. These ground deformations are explained by the inflation and deflation of a Mogi's source model (a point source model) located 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 pressure source during deflation. The horizontal displacements at the reference 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 pressure source. Based on the relation between the deformation volume of the ground surface and the discharged volume of the lava, it is estimated that during the eruption there was magma supply from the deeper portion as well as magma discharge at the crater. Magma is estimated to be supplied to the reservoir 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 Elsevier Science B.V. All rights reserved,.
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页码:23 / 34
页数:12
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