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Surface deformations associated with the October 2004 Mid-Niigata earthquake: Description and discussion

Earth, Planets and Space volume 57, pages 1093–1102 (2005)Cite this article

Abstract

The Mid-Niigata earthquakes (mainshock: JMA M6.8, the largest aftershock: JMA M6.4) occurred on 23 October 2004 in the Shinano River fold and thrust zone, western margin of Northeast Japan. Two major Quaternary reverse fault systems, fault related to Higashiyama—Tamguiyama fold in western side and Muikamachi fault in eastern side, had already been mapped in aftershock area from the geological structure and tectonic morphostructure. These active fault and fold strike almost north-northeast—south-southwest. We investigated destructions of man-made structures and surface deformation using the releveling data by Geography Survey Institute. In turn, we examined about the origin of observed surface destructions from the compare with aftershock distribution. Our leveling and G.S.I leveling results indicate the deformation concordant with the Higashiyama-Tamugiyama fold and the offset along the a part of the northern half of Muikamachi fault. The vertical displacements are estimated to be ca. 70 cm and less than 20 cm, respectively. The surface destructions were identified almost only along the Suwatoge flexure (correlated to the eastern limb of the Higashiyama-Tamugiyama fold), Tagawa anticline, Obiro fault and Muikamachi fault. The shortening amounts were estimated to be ca. 16 cm at the Suwatoge flexure, less than 2 cm at the Tagawa anticline and ca. 8 cm at the Muikamachi fault from the compressional destruction of man-made structure. The maximum vertical displacement and shortening was appeared at the bottom of Suwatoge flexure. The Suwatoge flexure is located onto the shallower extension of the row of aftershocks which was correlated to main shock earthquake. The Muikamachi fault is located near the shallower extension of the source fault of the largest aftershock. The stress regime inferred from the character of the observed surface destructions is concordant with the trend of geological structure and focal mechanism solutions. The small compressional destructions of man-made structures are byproducts created by buried faulting and folding. Thus, the Higashiyama-Tamugiyama folding structure grew in association with the buried faulting in the 2004 earthquake.

References

  • Aoki, S., M. Nishi, K. Nakamura, T. Hashimoto, S. Yoshikawa, and H. M. Ito, Multi-planar structures in the aftershock distribution of the Mid Niigata prefecture Earthquake in 2004, Earth Planets Space, 57, 411–416, 2005.

    Article  Google Scholar 

  • Asano, K. and T. Iwata, Source process of the 2004 Mid Niigata Prefecture earthquake estimated from the waveform inversion of strong motion records, 2005 Joint Meeting for Earth and Planetary Science, abstract, S079P–007, 2005 (in Japanese with English abstract).

    Google Scholar 

  • Fusejima, Y., T. Yoshioka, K. Mizuno, M. Shishikura, R. Imura, T. Komatsubara, and T. Sasaki, Surface ruptures associated with the 2000 Tottori-ken Seibu earthquake, G.S.J. Annual Report on Active Fault and Paleoearthquake Researches, 1, 1–26, 2001 (in Japanese).

    Google Scholar 

  • Hikima, K. and K. Koketsu, Source processes of the Mid Niigata Prefecture earthquakes in 2004 inferred from strong motion data, 2005 Joint Meeting for Earth and Planetary Science, abstract, S101–016, 2005 (in Japanese with English abstract).

    Google Scholar 

  • Hirata, N., H. Sato, S. Sakai, A. Kato, and E. Kurashimo, Fault system of the 2004 Mid Niigata Prefecture Earthquake and its aftershocks, Landslides, 2, doi:10.1007/s10346-005-0050-8, 2005.

  • Honda, R., S. Aoi, N. Morikawa, H. Sekiguchi, T. Kunugi, and H. Fujiwara, Ground motion and rupture process of the 2004 Mid Niigata Prefecture earthquake obtained from strong motion data of K-NET and KiK-net, Earth Planets Space, 57, 527–532, 2005.

    Article  Google Scholar 

  • Ikeda, Y., The origin and mechanism of active folding in Japan, Active Fault Research (Katsudanso Kenkyu), 22, 67–70, 2002 (in Japanese with English abstract).

    Google Scholar 

  • Kato, A., E. Kurashimo, N. Hirata, T. Iwasaki, and T. Kanazawa, Imaging the source region of the 2004 Mid-Niigata prefecture earthquake and the evolution of a seismogenic thrust-related fold, Geophys. Res. Lett., doi: 10.1029/2005GL022366, 2005a.

    Google Scholar 

  • Kato, A., S. Sakai, N. Hirata, E. Kurashimo, S. Nagai, T. Iidaka, T. Igarashi, Y. Yamanaka, S. Murotani, T. Kawamura, T. Iwasaki, and T. Kanazawa, Spatiotemporal variations of the aftershock distributions during one month after the occurrence of the 2004 mid-Niigata prefecture earthquake, Earth Planets Space, 57, 551–556, 2005b.

    Article  Google Scholar 

  • Kato, N., T. Echigo, H. Sato, M. Tateishi, S. Ogino, S. Sakai, S. Toda, S. Koshiya, T. Ito, T. Toyoshima, T. Imaizumi, H. Kato, and S. Abe, Geologic fault model based on High-resolution seismic reflection profiling across the surface rupture associated with the 2004 Mid-Niigata Prefecture earthquake (M6.8), central Japan, Earth Planets Space, 57, 447–452, 2005.

    Article  Google Scholar 

  • Kim, H. Y., Active faults along the western margin of the Muikamachi Basin, central Japan, Quaternary Research (Daiyonki Kenkyu), 40, 161–168, 2001 (in Japanese with English abstract).

    Article  Google Scholar 

  • Kim, H. Y., Relationship between the upheaval process of the Uonuma Hills and the cumulative nature of the Muikamachi fault, central Japan, Active Fault Research (Katsudanso Kenkyu)24, 63–75, 2004 (in Japanese with English abstract).

    Google Scholar 

  • Korenaga, M., S. Matsumoto, Y. Iio, T. Matsushima, K. Uehira, and T. Shibutani, Three dimensional velocity structure around aftershock area of the 2004 Niigata-ken Chuetsu Earthquake (M6.8) by the Double- Difference tomography, Earth Planets Space, 57, 429–433, 2005.

    Article  Google Scholar 

  • Maruyama, T., Y. Fusejima, T. Yoshioka, Y. Awata, and T. Matsu’ura, Characteristics of surface rupture associated with the 2004 Mid Niigata Prefecture earthquake, central Japan and their seismotectonic implications, Earth Planets Space, 57, 521–526, 2005.

    Article  Google Scholar 

  • Matsuda, T., Magnitude and recurrence interval of earthquakes from a fault, J. Seis. Soc. Jap. (Zisin), 28, 269–283, 1975 (in Japanese with English abstract).

    Google Scholar 

  • Mizoue, M., K. Nakamura, and S. Izutsuya, Mode of vertical crustal movements as deduced from the precise relevelings in the Ojiya active folding area, Niigata Prefectrure, Northeast Japan, Bull. Earthq. Res. Inst., 55, 199–224, 1980 (in Japanese with English abstract).

    Google Scholar 

  • Mizoue, M., T. Yokota, and I. Nakamura, High angle reverse faulting in the interaxial zone of active folds in the inner belt of Northeast Japan, Bull. Earthq. Res. Inst., 57, 359–377, 1982 (in English with Japanese abstract).

    Google Scholar 

  • Mori, J. and P. Somerville, 2004 Niigata-ken Chuetsu Earthquake— Seismology and strong ground motions, Earthquake Engineering Research Institute, 2005 (submitted).

    Google Scholar 

  • Nakamura, K. and Y. Ota, Study of active fold in Japan, a review, Quaternary Research (Daiyonki Kenkyu), 7, 200–211, 1968 (in Japanese with English abstract).

    Article  Google Scholar 

  • Namegaya, Y., Y. Tsuji, and J. Ito, Detailed distributions of seismic intensities of the 1828 Bunsei Echigo-Sanjo and the 1751 Horeki Echigo- Takada earthquakes, 2005 Joint Meeting for Earth and Planetary Science, abstract, J027–011, 2005 (in Japanese with English abstract).

    Google Scholar 

  • Okada, T., N. Umino, T. Matsuzawa, J. Nakajima, N. Uchida, T. Nakayama, S. Hirahara, T. Sato, S. Hori, T. Kono, Y. Yabe, K. Ariyoshi, S. Gamage, J. Shimizu, J. Suganomata, S. Kita, S. Yui, M. Arao, S. Hondo, T. Mizukami, H. Tsushima, and T. Yaginuma, Aftershock distribution and 3D seismic velocity structure in and around the focal area of the 2004 mid Niigata earthquake obtained by applying doubledifference tomography to dense temporary seismic network data, Earth Planets Space, 57, 435–440, 2005.

    Article  Google Scholar 

  • Ota, Y., Crustal movements in the late Quaternary considered from the deformed terrace plains in northeastern Japan, Japanese J. Geol. Geophys., 40, 41–61, 1969.

    Google Scholar 

  • Otsuka, Y., Active rock folding in Japan, Proc. Imp. Acad. Japan, 13, 78–81, 1941 (in Japanese).

    Google Scholar 

  • Sagiya, T., S. Miyazaki, and T. Tada, Continuous GPS array and presentday crustal deformation of Japan, PAGEOPH, 157, 2303–2322, 2000.

    Google Scholar 

  • Sakai, S., N. Hirata, A. Kato, E. Kurashimo, T. Iwasaki, and T. Kanazawa, Multi-fault system of the 2004 Mid-Niigata Prefecture Earthquake and its aftershocks, Earth Planets Space, 57, 417–428, 2005.

    Article  Google Scholar 

  • Sato, H., The relationship between late Cenozoic tectonic events and stress fields and basin development in northeast Japan, J. Geophys. Res., 99, 22261–22274, 1994.

    Article  Google Scholar 

  • Sato, H. and N. Kato, Relationship between geologic structure and the source fault of the 2004 Mid-Niigata Prefecture Earthquake, central Japan, Earth Planets Space, 57, 453–457, 2005.

    Article  Google Scholar 

  • Shibutani, T., Y. Iio, S. Matsumoto, H. Katao, T. Matsushima, S. Ohmi, F. Takeuchi, K. Uehira, K. Nishigami, B. Enescu, I. Hirose, Y. Kano, Y. Kohno, M. Korenaga, Y. Mamada, M. Miyazawa, K. Tatsumi, T. Ueno, H. Wada, and Y. Yukutake, Aftershock distribution of the 2004 Mid Niigata Prefecture Earthquake derived from a combined analysis of temporary online observations and permanent observations, Earth Planets Space, 57, 545–549, 2005.

    Article  Google Scholar 

  • Shimazaki, K., Small and large earthquakes: the effects of the thickness of seismogenic layer and the free surface, in Earthquake Source Mechanics, AGU Monograph, 37 (Maurice Ewing Ser. 6), edited by S. Das, J. Boaghtwright, and C. H. Sholz, pp. 209–216, 1986.

    Chapter  Google Scholar 

  • Shirai, T., Crustal movement during the Late Quaternary along the lower course of the Uono River, Niigata Pref., Japan. Bull. Geography, Tokyo Edu. Univ., 11, 23–35, 1967 (in Japanese).

    Google Scholar 

  • Suzuki, Y., M. Watanabe, and D. Hirouchi, Surface earthquake fault of the Mid Niigata Prefecture earthquake in 2004, Journal of Geography (Chigaku Zassi), 113, 861–870, 2004 (in Japanese with English abstract).

    Article  Google Scholar 

  • Watanabe, M., Y. Suzuki, H. Tsutsumi, H. Y. Kim, and H. Sato, 1:25,000 Active Fault Map in Urban Area [Oziya district], Geographical Survey Institute of Japan, 2001 (in Japanese).

  • Yagi, Y., Source process of the 2004 Mid Niigata Prefecture earthquake obtained by joint inversion of near-field and teleseismic, 2005 Joint Meeting for Earth and Planetary Science, abstract, S101P–001, 2005 (in Japanese with English abstract).

    Google Scholar 

  • Yamanaka, Y., EIC seismological note, no. 154, http://www.eri.u-tokyo.ac.jp/sanchu/SeismoNote/, 2004.

  • Yanagisawa, Y., I. Kobayashi, K. Takeuchi, M. Tateishi, K. Tihara, and S. Kato, Geology of the Oziya District, With geological sheet map at 1:50,000, Geological Survey Institute of Japan, 177 pp., 1986 (in Japanese with English abstract).

    Google Scholar 

  • Yeats. R. S., Fault related to folding with examples from New Zealand, Royal. Soc., New Zealand Bull., 24, 273–292, 1986.

    Google Scholar 

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Authors and Affiliations

  1. Earthquake Research Institute, University of Tokyo, 113-0032, Japan

    Kim Haeng Yoong

  2. Division of Earth and Planetary Sciences, Kyoto University, 606-8502, Japan

    Atsumasa Okada

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  1. Kim Haeng Yoong
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  2. Atsumasa Okada
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Correspondence to Kim Haeng Yoong.

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Yoong, K.H., Okada, A. Surface deformations associated with the October 2004 Mid-Niigata earthquake: Description and discussion. Earth Planet Sp 57, 1093–1102 (2005). https://doi.org/10.1186/BF03351888

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