1998Journal of Structural and Construction Engineering (Transactions of AIJ)Open access

CHARACTERISTICS OF THE GROUND MOTION OF THE 1997 KAGOSHIMAKEN-HOKUSEIBU EARTHQUAKE

Kazuo Matsumura

Open full text 2 citations

Abstract

The earthquakes which occurred in the northwestern part of Kagoshima prefecture on March 26 and May 13 in 1997 caused severe damage to some reinforced concrete school buildings and wooden houses. Many ground motion records are obtained by the seismographs of JMA and NIED which settled in high density after 1995 Hyogoken-Nanbu Earthquake. The response spectra of the ground motion of four sites which surround the seismic region are analyzed. The large peak ground accelerations such as 728 cm/s^2 at Izumi or 902 cm/s^2 at Miyanojyo are recorded but did not cause no severe damage of buildings near seismographs. These records contain predominant high frequencies of over 5 Hz. The response spectra of four sites are different by the location to the seismic region.

Open-access reader

About this research paper

What this paper is about

The earthquakes which occurred in the northwestern part of Kagoshima prefecture on March 26 and May 13 in 1997 caused severe damage to some reinforced concrete school buildings and wooden houses. Many ground motion records are obtained by the seismographs of JMA and NIED which settled in high density after 1995 Hyogoken-Nanbu Earthquake. The response spectra of the ground motion of four sites which surround the seismic region are analyzed. The large peak ground accelerations such as 728 cm/s^2 at Izumi or 902 cm/s^2 at Miyanojyo are recorded but did not cause no severe damage of buildings near seismographs. These records contain predominant high frequencies of over 5 Hz. The response spectra of four sites are different by the location to the seismic region.

Why it matters

OpenAlex reports 2 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

The earthquakes which occurred in the northwestern part of Kagoshima prefecture on March 26 and May 13 in 1997 caused severe damage to some reinforced concrete school buildings and wooden houses. Many ground motion records are obtained by the seismographs of JMA and NIED which settled in high density after 1995 Hyogoken-Nanbu Earthquake. The response spectra of the ground motion of four sites which surround the seismic region are analyzed. The large peak ground accelerations such as 728 cm/s^2 at Izumi or 902 cm/s^2 at Miyanojyo are recorded but did not cause no severe damage of buildings near seismographs. These records contain predominant high frequencies of over 5 Hz. The response spectra of four sites are different by the location to the seismic region.

Key concepts: Seismometer, Seismology, Ground motion, Geology, Peak ground acceleration, Seismic microzonation, Geodesy

Related papers

Back to paper searchBrowse research topicsOriginal source
CHARACTERISTICS OF THE GROUND MOTION OF THE 1997 KAGOSHIMAKEN-HOKUSEIBU EARTHQUAKE — Research Paper | ScholarLens