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Seismologische Grundlagen

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Die Wirkungskette seismischer Phänomene (Bild 2–1) besteht aus drei Gliedern, dem Entstehungsort seismischer Wellen, dem Ausbreitungsmedium und dem Einwirkort. Jedes der drei Glieder der Kette prägt den zeitlichen Verlauf und die Stärke der Erschütterungen, die letztendlich ein Bauwerk dynamisch belasten.

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(2007). Seismologische Grundlagen. In: Bauwerke und Erdbeben. Vieweg. https://doi.org/10.1007/978-3-8348-9161-7_2

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