Transient crustal deformation in Tokai region, central Japan, until May 2004
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- Ozawa Shinzaburo
- Geography and Crustal Dynamics Research Center, Geographical Survey Institute of Japan
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- Murakami Makoto
- Geography and Crustal Dynamics Research Center, Geographical Survey Institute of Japan
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- Kaidzu Masaru
- Geography and Crustal Dynamics Research Center, Geographical Survey Institute of Japan
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- Hatanaka Yuki
- Geography and Crustal Dynamics Research Center, Geographical Survey Institute of Japan
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説明
An analysis of Global Positioning System (GPS) data reveals a continuation of the transient crustal deformation that was first reported by Ozawa et al. (2002) in the western Tokai region. Kalman filtering following the timedependent inversion shows a slow-thrust slip occurring on the plate boundary in the western Tokai region, with its center around Lake Hamana, which is adjacent to the anticipated Tokai earthquake source area. The moment release from the Tokai silent earthquake was observed to be continuous surpassing Mw 7.0 in May 2004, with relative slip increases to the northeast and north of Lake Hamana from 2002. The moment release rate decreased in 2002, and then increased in 2003, reaching the rate observed in 2001.
収録刊行物
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- Earth, Planets and Space
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Earth, Planets and Space 57 (10), 909-915, 2005
地球電磁気・地球惑星圏学会 、公益社団法人 日本地震学会、特定非営利活動法人 日本火山学会、日本測地学会、日本惑星科学会
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詳細情報 詳細情報について
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- CRID
- 1390001206513093632
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- NII論文ID
- 10017470338
- 130003781070
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- NII書誌ID
- AA11211921
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- ISSN
- 18805981
- 13438832
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- NDL書誌ID
- 7687714
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
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- CiNii Articles
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