Summary
Near-source seismic strong-motion records are controlled by source effects. Using a source inversion method, however, the true solution is not recovered, and the goodness of recovery much depends upon station array. The resolving power of station array is measured, and the optimum array geometry is determined.
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© 1993 Springer-Verlag Berlin Heidelberg
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Iida, M. (1993). Optimum Strong-Motion Station-Array Geometry for Earthquake Source Studies. In: Tanaka, M., Bui, H.D. (eds) Inverse Problems in Engineering Mechanics. International Union of Theoretical and Applied Mechanics. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-52439-4_40
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DOI: https://doi.org/10.1007/978-3-642-52439-4_40
Publisher Name: Springer, Berlin, Heidelberg
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