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The two-station method was first introduced by Sato 1955.
(b) Hypocenters relocated using the homogeneous station method.
Fig. 2 Schematic diagram of the two-station method.
In addition, the fundamental periods of the station sites were estimated by the single station method.
This data was used to estimate site amplifications by the reference-station method.
An advantage of the single-station method is that information on earthquakes is quickly obtained.
First, we eliminated the Sq contribution at the dip equator by using a two-station method.
This suggests that the single station method works well in the Mt. Kinabalu area (Fig. 2b).
In general, earthquake information estimated from the single station method is obtained more quickly, and, yet, with a lower accuracy compared with that estimated from the multi-station method.
In the rest of this paper, we use the EEJ defined by the two-station method for further investigation.
We have adopted the EEJ obtained by the use of the two-station method for our study.
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