期刊
EARTH PLANETS AND SPACE
卷 60, 期 12, 页码 1197-1201出版社
SPRINGER HEIDELBERG
DOI: 10.1186/BF03352878
关键词
2008 Iwate-Miyagi Nairiku earthquake; kinematic GPS; coseismic fault model
资金
- Young Scientists Research of Japan Society for the Promotion of Science [19840006]
A large earthquake of M-j 7.2 occurred on June 14, 2008, beneath the border between Iwate and Miyagi pre-fectures in northeastern Japan. We propose a simple rectangular fault model based on a dense GPS network, including continuous GPS sites run by four agencies, to describe the coseismic deformation. The coseismic displacements are estimated by kinematic PPP (precise point positioning) analysis. Near the hypocenter, co-located independent instruments (integrated accelerogram and kinematic PPP) measure the same large displacement caused by the mainshock. The fault model explains the observations well and reproduces the observed complex spatial pattern, especially around the northern part of the focal area, which is the focus of a debate on whether or not the coseismic slip occurred on the Dedana fault system. Our results show that no major slip on the Dedana fault system occurred. The estimated amount of moment release wits equivalent to M-w, 6.9, and the maximum slip reached 3.5 m on the southern sub-fault.
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