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.
８－２ 近畿・四国地方の地殻変動
Crustal Movements in Kinki and Shikoku Districts Geographical Survey Institute 122311241 222311-1 2 34 BM9189 12 4BM4772 251-2 5 2495 6 251 7 51635121 8 91219 1 1118 12112 13GEONET1622 249241264-496 -
（1809） 桜島火山における多項目観測に基づく火山噴火準備過程解明のための研究
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４－２ 伊豆地方の地殻変動
4-2 伊豆地方の地殻変動 Crustal Movements in the Izu penimsula and its Visinity 国土地理院 Geographical Survey Institute 第 1~12 図は 伊豆半島およびその周辺における水準測量結果である 1998 年以前は伊東付近が継続的に隆起していたが 1998 年以降はその隆起がほぼ止まっていた 最近 2002 年 5
Fig. 1. Horizontal displacement of the second and third order triangulation points accompanied with the Tottori Earthquake of (after SATO, 1973)
Journal of the Geodetic Society of Japan Vol. 27, No. 3, (1981), pp. 183-191 Research on Fault Movement by means of Aero-Triangulation ( T) (An experiment on the earthquake fault of the Izu-Oshima Kinkai
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* Coseismic and postseismic coastal environment changes caused by the 1703 Genroku Kanto Earthquake in the southern part of Boso Peninsula, central Japan Jun Muragishi Graduate School of Urban Environmental
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20 * Re-Evaluation of Isoseismal Maps and Magnitudes from Two Big Earthquakes along the Subduction Zone of Kyushu and Ryukyu Islands Early in the 20th Century Masayuki TAKEMURA, Katsuhisa KANDA Kobori
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Structure of the Basement and the Gravity Anomaly in the Kanto Plain -A Geophysical Study of Active Fault- Takashi TADA Crustal Dynamics Department, Geographical Survey Institute (Received Apirl 7, 1983)
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60 547 547 4km [ ] 14 20 18 2,400 5,500 24 15 10,000 [ ] [ ] 1779 1779 1471-76 1914 1471-76 1779 1914 1779 1779 1914 1471-7676 1779 1471-76 1946 1914 59 8 25 30 1986 3km 2m 5 2km 18 6 [ ]
1,000m 875m1 6km
1,000m 875m1 6km 1,000m 875m 30 13 14 11 2 14 23 27 50 30 3 () 23 24 25 16,534 16,792 18,017 13,946 17,884 18,712 30,480 34,676 36,729 1 (25 ) () 395 1,420 1,343 1,756 1,364 1,599 1,184 1,278 1,619 1,324
私にとっての沖縄と独自性.PDF
6902117 2 1200km 48 11 46 36 40 (1) ( ) 3 1 1-1 1-2 2 (= ) 3 1. 14 14 ( ) ( 2001) ( ) ( ) 1390 1474 ( 2001) ( 4 ) ( ) 46 3000 ( ) = 5 1609 1602 ( 2001) 1-1 1-2 1-1 1-2 15 (2) 6 1314 ( ) (3) ( ) 1 ( 1993:48)
阪神５年PDF.PDF
1995.1.17 N 0km 10 20 31 4,569 14,679 67,421 55,145 6,965 80 1,471 3,383 13,687 5,538 327 22 933 1,112 12,757 5,675 465 2 243 3,782 6,344 6,641 65 17 555 1,755 9,533 8,109 940 15 12 817 271 3,140 1 918