8-5 中国・四国・九州地方の地殻変動
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1 Crustal Movements in the Chugoku, Shikoku and Kyushu Districts Geographical Survey Institute 1 -(1) (9)GPS (Mj7.3) 2 co-seismic (1) (6) 5 -(1) (3) 2001 GPS 6 7 GPS (1) (4) GPS 9
2 1 -(1) GPS(1) Fig.1-(1) Results of continuous GPS measurements in the western part of Tottori prefecture during 1998/01/ /04/21 (1 of 9).
3 1 -(2) GPS(2) Fig.1-(2) Results of continuous GPS measurements in the western part of Tottori prefecture during 1998/01/ /04/21 (2 of 9).
4 1 -(3) GPS(3) Fig.1-(3) Results of continuous GPS measurements in the western part of Tottori prefecture during 1998/01/ /04/21 (3 of 9).
5 1 -(4) GPS(4) Fig.1-(4) Results of continuous GPS measurements in the western part of Tottori prefecture during 1998/01/ /04/21 (4 of 9).
6 1 -(5) GPS(5) Fig.1-(5) Results of continuous GPS measurements in the western part of Tottori prefecture during 1998/01/ /04/21 (5 of 9).
7 1 -(6) GPS(6) Fig.1-(6) Results of continuous GPS measurements in the western part of Tottori prefecture during 1998/01/ /04/21 (6 of 9).
8 1 -(7) GPS(7) Fig.1-(7) Results of continuous GPS measurements in the western part of Tottori prefecture during 1998/01/ /04/21 (7 of 9).
9 1 -(8) GPS(8) Fig.1-(8) Results of continuous GPS measurements in the western part of Tottori prefecture during 1998/01/ /04/21 (8 of 9).
10 1 -(9) GPS(9) Fig.1-(9) Results of continuous GPS measurements in the western part of Tottori prefecture during 1998/01/ /04/21 (9 of 9).
11 2 Fig.2 Horizontal displacements in the western part of Tottori prefecture derived from repeated surveys before and after 2000 Tottoriken Seibu Earthquake.
12 3 Fig.3 Vertical displacements in the Chugoku district derived from repeated precise leveling surveys before and after 2000 Tottoriken Seibu Earthquake.
13 4 -(1) (1) Fig.4-(1) Horizotal strain in the northern Kyushu and San'in districts derived from repeated surveys (1 of 6).
14 4 -(2) (2) Fig.4-(2) Horizotal strain in the northern Kyushu and San'in districts derived from repeated surveys (2 of 6).
15 4 -(3) (3) Fig.4-(3) Horizotal strain in the northern Kyushu and San'in districts derived from repeated surveys (3 of 6).
16 4 -(4) (4) Fig.4-(4) Horizotal strain in the northern Kyushu and San'in districts derived from repeated surveys (4 of 6).
17 4 -(5) (5) Fig.4-(5) Horizotal strain in the northern Kyushu and San'in districts derived from repeated surveys (5 of 6).
18 4 -(6) (6) Fig.4-(6) Horizotal strain in the northern Kyushu and San'in districts derived from repeated surveys (6 of 6).
19 5 -(1) GPS(1) Fig.5-(1) Results of continuous GPS measurements around the epicenter of 2001 Geiyo earthquake during 1998/01/ /04/21 (1 of 3).
20 5 -(2) GPS(2) Fig.5-(2) Results of continuous GPS measurements around the epicenter of 2001 Geiyo earthquake during 1998/01/ /04/21 (2 of 3).
21 5 -(3) GPS(3) Fig.5-(3) Results of continuous GPS measurements around the epicenter of 2001 Geiyo earthquake during 1998/01/ /04/21 (3 of 3).
22 Fig.6 Horizontal displacements associated with 2001 Geiyo earthquake (March 24, 2001 Mj6.4) derived from continuous GPS measurements.
23 Fig.7 Vertical displacements associated with 2001 Geiyo earthquake (March 24, 2001 Mj6.4) derived from continuous GPS measurements.
24 GEONET Mj 3/ cm mm kmkm Mw6.7 Hirose et al. 1999, Ozawa et al km Ozawa et al. [2001]
25 8 -(1) 2001(1) Fig.8-(1) Interpretations of crustal deformation associated with 2001 Geiyo earthquake (1 of 3).
26 8 -(2) 2001(2) Fig.8-(2) Interpretations of crustal deformation associated with 2001 Geiyo earthquake (2 of 3).
27 第 8 図 -(3) 2001 年芸予地震に伴う地殻変動 (3) Fig.8-(3) Interpretations of crustal deformation associated with 2001 Geiyo earthquake (3 of 3) -6-
28 9 Fig.9 Plots of differences between montly mean values at tidal gauges in the central part of Setonaikai inland ocean.
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