Estimation of the period of prehistoric large earthquake occurrence along the Senya fault system in Tohoku District, northeast Japan.

S. I. Hirano

doi:10.4157/grj1984a.57.3_173

Estimation of the period of prehistoric large earthquake occurrence along the Senya fault system in Tohoku District, northeast Japan.

S. I. Hirano

Research output: Contribution to journal › Article › peer-review

1 Citation (Scopus)

Abstract

The Senya fault system is one of the most prominent active reverse faults in Japan. Prehistoric fault activities along the fault system have been revealed by observing the stratigraphy at fault outcrops. Seismic events of two different periods are inferred from fault activities shown by the geological and topographical evidences along the fault system. One is 1896 AD that is, Riku-u earthquake. The other event is estimated to have occurred after ca. 4400 yr BP, but before 2700 yr BP. -from English summary

Original language	English
Pages (from-to)	173-185
Number of pages	13
Journal	Geographical Review of Japan, Series A
Volume	57
Issue number	3
DOIs	https://doi.org/10.4157/grj1984a.57.3_173
Publication status	Published - 1984 Jan 1
Externally published	Yes

ASJC Scopus subject areas

Geography, Planning and Development
Earth-Surface Processes

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abstract = "The Senya fault system is one of the most prominent active reverse faults in Japan. Prehistoric fault activities along the fault system have been revealed by observing the stratigraphy at fault outcrops. Seismic events of two different periods are inferred from fault activities shown by the geological and topographical evidences along the fault system. One is 1896 AD that is, Riku-u earthquake. The other event is estimated to have occurred after ca. 4400 yr BP, but before 2700 yr BP. -from English summary",

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AB - The Senya fault system is one of the most prominent active reverse faults in Japan. Prehistoric fault activities along the fault system have been revealed by observing the stratigraphy at fault outcrops. Seismic events of two different periods are inferred from fault activities shown by the geological and topographical evidences along the fault system. One is 1896 AD that is, Riku-u earthquake. The other event is estimated to have occurred after ca. 4400 yr BP, but before 2700 yr BP. -from English summary

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Estimation of the period of prehistoric large earthquake occurrence along the Senya fault system in Tohoku District, northeast Japan.

Abstract

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