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Nansei Japan

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Journal Article
Published: 01 August 1997
Bulletin of the Seismological Society of America (1997) 87 (4): 904–917.
...Yasumaro Kakehi; Kojiro Irikura Abstract We investigate the process of high-frequency (1 to 10 Hz) radiation on the fault plane of the 1993 Hokkaido-Nansei-Oki, Japan, earthquake ( M W = 7.5) from the envelope inversion of strong-motion acceleration seismograms. For the analysis, empirical Green's...
Journal Article
Published: 01 April 1996
Bulletin of the Seismological Society of America (1996) 86 (2): 505–518.
...Keiko Kuge; Jiajun Zhang; Masayuki Kikuchi Abstract We present an analysis of the data dependency of surface-wave inversions for source parameters of the 12 July 1993 Hokkaido-Nansei-Oki, Japan, earthquake. This dependency is demonstrated by differences between source mechanisms obtained from...
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Modeled cumulative number of aftershocks for the Hokkaido‐<span class="search-highlight">Nansei</span>‐Oki, <span class="search-highlight">Japan</span>...
Published: 05 November 2013
Figure 12. Modeled cumulative number of aftershocks for the Hokkaido‐Nansei‐Oki, Japan, M s  7.8 earthquake of 12 July 1993 using equation  (35) . The leftmost, middle, and rightmost segments of the line signify aftershocks occurring before, during, and after the deployment of a pseudotemporary
Series: Society of Exploration Geophysicists Geophysical References Series
Published: 01 January 1998
EISBN: 9781560801832
... Abstract Aeromagnetic surveys offshore the western Nansei Islands, Japan, were conducted by the Geological Survey of Japan (GSJ) from 1982 to 1989 (Okuma et al., 1991). The surveys cover the area from the Tunghai Shelf in the East China Sea to the Okinawa Trough west of the Nansei Islands...
Journal Article
Journal: Elements
Published: 01 June 2022
Elements (2022) 18 (3): 187.
... and drifted westward, arriving at the Nansei Islands after two months of drifting. The pumice further drifted westward, arriving at the Philippines and Taiwan, as well as eastward, arriving at the Kanto area of eastern Japan. Although the Plinian eruption of FOB did not cause any direct disasters, the large...
Journal Article
Published: 01 December 2001
Bulletin of the Seismological Society of America (2001) 91 (6): 1898–1909.
...., 1995 ), the 1993 Hokkaido-nansei-oki, Japan earthquake ( Shuto, 1998 ), and more recently the 1998 Papua New Guinea earthquake ( Fujima et al., 1999 ; Matsuyama et al., 1999 ). In these instances, considerable discrepancy in tsunami arrival time and wave height has been pointed out between...
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Comparison of the spatial variation of the  C  (a) and  q  (b) values for t...
Published: 01 October 2005
Figure 10. Comparison of the spatial variation of the C (a) and q (b) values for the 1993 M 7.7 Hokkaido Nansei-Oki earthquake in Japan (event 15 in Table 1 ). A much sharper high-value peak close to the epicenter (solid circle) is observed for the q distribution.
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Variation of the cumulative Benioff strain for the narrower seismogenic sou...
Published: 01 October 2005
Figure 11. Variation of the cumulative Benioff strain for the narrower seismogenic source region of the 1993 M 7.7 Hokkaido Nansei-Oki earthquake in Japan (elliptical area in Fig. 10 ). A clear decelerating pattern is observed, in contrast to the accelerating deformation pattern of the broader
Journal Article
Published: 01 August 2008
Petroleum Geoscience (2008) 14 (3): 223–233.
... . A review of petroleum system in the deep water area of the Toyama Trough to the Sado Island in the Japan Sea, based on the results of the METI Sado Nansei Oki drilling . Journal of the Japanese Association for Petroleum Technology , 71 , 618 – 627 [in Japanese with English abstract]. Nakayama...
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(a) Inset map showing the location of the source region in <span class="search-highlight">Japan</span>. (b) Distr...
Published: 01 February 2001
Figure 1. (a) Inset map showing the location of the source region in Japan. (b) Distribution of epicenters (gray circles) from March 26 to September 30, 1997, and strong-motion stations (reversed triangles) used in this study. The stars stand for the epicenters of the two large earthquakes
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Major tsunami events in <span class="search-highlight">Japan</span>             Name  Year  Number of Casualties ...
Published: 01 March 2013
Table 1 Major tsunami events in Japan Name Year Number of Casualties and Missing People Meiji Sanriku Earthquake Tsunami 1896 Approximately 22,000 Showa Sanriku Earthquake Tsunami 1933 3,064 Tonankai Earthquake 1944 1,223 Nankai Earthquake 1946 1,443 Chile
Journal Article
Published: 01 October 1995
Bulletin of the Seismological Society of America (1995) 85 (5): 1343–1358.
... , 481 - 490 . Nakanishi I. Kikuchi M. (1993) . Characteristics of the 1993 Hokkaido-Nansei-Oki earthquake , J. Japan Soc. Earthquake Eng. Promotion ( NEWS ) , no. 133 , 1 - 5...
Journal Article
Published: 01 June 2001
Bulletin of the Seismological Society of America (2001) 91 (3): 604–616.
... ). Kyoshin Net (K-NET) , Seism. Res. Lett . 69 , 309 – 332 . Kuge , K. , J. Zang , and M. Kikuchi ( 1996 ). The 12 July 1993 Hokkaido-Nansei-Oki, Japan, earthquake: effects of source complexity on surface-wave radiation , Bull. Seism. Soc. Am . 86 , 505 – 518 . Matuzawa , T...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1959
AAPG Bulletin (1959) 43 (2): 381–396.
...Godfrey F. Kaufmann ABSTRACT The tectonic framework of the northwest quadrant of the circum-Pacific orogenic belt is explained as the result of the process postulated in the theory of growing continental masses. The festoons of island arcs marked by the Nampo Shoto, Northern Japan, the Kuriles...
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Journal Article
Published: 01 May 2001
Seismological Research Letters (2001) 72 (3): 362–366.
... of the computation, as demonstrated by the satisfactory prediction of run-up during the extreme inundation flows of the Hokkaido-Nansei-Oki tsunami of 1993 ( Titov and Synolakis, 1997 ). Based on these two paragraphs, the predictions of these inundation codes cannot be discarded outright in favor of analytical...
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Development of completeness magnitudes for four selected regions: Tohoku, K...
Published: 06 February 2018
Figure 4. Development of completeness magnitudes for four selected regions: Tohoku, Kanto, Kinki, and mainland Japan. Solid blue, yellow, and red lines indicate the 99th percentile of the distribution of all completeness magnitudes M P | P = 0.99 over space, for depth levels
Journal Article
Published: 01 May 1997
Seismological Research Letters (1997) 68 (3): 386–400.
.... Satake ( 1996 ). The Sanriku-oki, Japan, earthquake of December 28, 1994 ( M w 7.7): Rupture of a different asperity from a previous earthquake , Geophys. Res. Lett ., 23 , 1,465 – 1,468 . Tanioka , Y. and L. J. Ruff ( 1996 ). The October 9th 1995 Jalisco earthquake, (abs...
Journal Article
Published: 21 July 2021
Seismological Research Letters (2021) 92 (6): 3610–3625.
... for ordinary seafloor observations of local earthquakes. Observation of slow earthquakes, especially VLFEs, requires a broadband seismic sensor. The Nankai trough region (Fig.  1 ), where the Philippine Sea plate is subducting below the southwestern Japan archipelago, is known to have high activities...
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Journal Article
Published: 01 October 1996
Bulletin of the Seismological Society of America (1996) 86 (5): 1229–1237.
... , Washington D.C. , 579 - 592 . Mendoza C. Fukuyama E. (1996) . The July 12, 1993, Hokkaido-Nansei-Oki, Japan, earthquake: coseismic slip pattern from strong-motion and teleseismic...
Journal Article
Published: 01 April 1998
Bulletin of the Seismological Society of America (1998) 88 (2): 609–620.
.... A. (1993) . Laboratory measurements of tsunami run-up . Tsunami '93 Proceedings , Wakayama , Japan , 585 - 598 . Briggs M. J. Synolakis C. E. Harkins G...