Evaluation of existing ground motion attenuation models for the application in Peninsular Malaysia

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Date
2014
Authors
Tze Che, Van
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Abstract
Peninsular Malaysia is considered a low seismicity region. A ground motion attenuation model that can best estimates peak ground acceleration (PGA) is essential prior in conducting seismic hazard assessment. With the scarcity of historical data, an attenuation model is difficult to be developed for Peninsular Malaysia. Therefore, the present research focuses on the comparison of 28 ground motion attenuation models with actual ground motion records in Peninsular Malaysia. These models are developed for subduction earthquakes and shallow crustal earthquakes in both active tectonic regions and stable continental regions. A total of 318 seismic records from 42 distant subduction and strike-slip Sumatra earthquakes with moment magnitude ranging from 5.2 to 9.0 spanning in a distance range of 284 km to 1292 km were obtained from 19 seismic stations operated by Malaysian Meteorological Department (MMD). Field survey was carried out to characterise the soil condition at those seismic stations using multi-channel analyses of surface waves (MASW). Normalised root mean squared error (RMSENor) values were calculated to provide quantitative measure of how well attenuation models predict ground motions. The result shows that Nabilah and Balendra (2012), Fukushima and Tanaka (1990) and Megawati and Pan (2010) models predict PGA close to the recorded data with Nabilah and Balendra (2012) having the lowest RMSENor value for distant subduction earthquakes. Suitable attenuation models for Peninsular Malaysia based on actual data utilised in this study in predicting ground motions for distant strikeslip earthquakes are Si and Midorikawa (2000) and Somerville et al. (2004) models.
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