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A connected graph which contains no circuits is a tree A node of a tree is a leaf if its degree is equal to 1 A directed graph (digraph) G is a pair (V, E ) , where E is a finite family of ordered pairs of elements of V Such graphs are frequently represented using arrows to represent edges In the directed graph here, the edge set is E = { ( a ,a), ( a ,b ) , (b,a ) , (b,a ) , ( a , c ) , (b,c), (c, 4 ,(d, 41..

by considering the directions in which the seismic waves left the focal region, as it is apparent that compressions and dilations are restricted to certain angular ranges A focal mechanism solution is obtained rstly by determining the location of the focus by the method outlined in Section 214 Then, for each station recording the earthquake, a model for the velocity structure of the Earth is used to compute the travel path of the seismic wave from the focus to the station, and hence to calculate the direction in which the wave left the focal region These directions are then plotted, using an appropriate symbol for compressional or dilational rst motion, on an equal area projection of the lower half of the focal sphere, that is, an imaginary sphere of small but arbitrary radius centered on the focus (Fig 25).

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An equal area net, which facilitates such a plot, is illustrated in Fig 26 The scale around the circumference of such a net refers to the azimuth, or horizontal component of direction, while dips are plotted on the radial scale from 0 at the perimeter to 90 at the center Planes through the focus are represented on such plots by great circles with a curvature appropriate to their dip; hence a diameter represents a vertical plane Let us assume that, for a particular earthquake, the fault motion is strike-slip along a near vertical fault plane This plane and the auxiliary plane plot as orthogonal great circles on the projection of the focal sphere, as shown on Fig 27.

June 12, 2004

The lineation de ned by the intersection of these planes is almost vertical, so it is apparent that the direction of movement along the fault is orthogonal to this intersection, that is, near horizontal The two shaded and two unshaded regions of the projection de ned by the nodal planes now correspond to the directions in which compressional and dilational.

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