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Rupture process at the beginning of the 2007 Chuetsu oki, Niigata, Japan, earthquake

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Figure

Fig. 3(a) has a minimum around the azimuth of N200◦and a maximum at an azimuth 180E◦ apart from the min-
Fig. 3(a). In the next section we examine the subsequent
Fig. 5.Vertical cross-section along the NW-SE direction. Two possiblemodels for the rupture propagation at the beginning main rupture stage.The bold line in each model indicates the fault plane where the rupturepropagates at the beginning stage of the main
Fig. 8.Geographical configuration of the hypocenter, the main ruptureonset position, and the imaged “asperities”

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