Construct · 1 fields · 2 citations
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A focal mechanism (or fault-plane solution) describes the orientation of the fault and the direction of slip in an earthquake, inferred from the pattern of first motions and wave amplitudes recorded around it. It is summarised by the familiar 'beachball' diagram, whose shaded and unshaded quadrants show where the ground first moved outward versus inward, and whose two nodal planes give the fault plane and an auxiliary plane. Aki and Richards's Quantitative seismology and Stein and Wysession's An introduction to seismology, earthquakes, and earth structure set out how it is derived from the radiation pattern or the moment tensor. The referent is the slip geometry of a seismic source, used to classify faulting as normal, reverse, or strike-slip.[1][2]
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