Horizontal Strain Rates in the Japanese Islands during interseismic period deduced from Geodetic Surveys (Part I)

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Towards inferring earthquake patterns from geodetic observations of interseismic coupling

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S1 An example of shear stress evolution in the VS patch during coseismic slip. Shear stress τ with respect to a reference stress value foσ̄ at the center of the VS patch (x = 120 km) is shown as a function of the coseismic slip of event 20 in Fig. 2b. The open circle indicates the stress τ i vs before the arrival of the dynamic rupture. The open triangle shows the peak shear stress τ vs. The ope...

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ژورنال

عنوان ژورنال: Zisin (Journal of the Seismological Society of Japan. 2nd ser.)

سال: 1990

ISSN: 0037-1114,1883-9029,2186-599X

DOI: 10.4294/zisin1948.43.1_13