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Fast Orientation: Menlo Park, Calif.
Conclusion The prehospital care of pediatric patients with severe trauma, taken in charge by the TRENAU, enables guidelines compliance in several points (fast orientation to adapted trauma center, duration of prehospital care).
The results suggest a detached slab as the deeper layer with NE SW fast orientation.
East West fast orientation are detected for station KBA, JAVS and CEY as well (Fig. 2).
The NE SW fast orientation at longitudes less than ∼12°E cannot be related to the high-velocity anomaly alone (cold lithospheric slab) since we observed the same fast orientation outside of the high-velocity body.
They clearly show the rotating pattern of fast orientation along the Alps previously described (seen in Fig. 2).
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Further to the East, the fast orientations turn from E W to NW SE, where the fast azimuth are predominantly N115° oriented.
Fig. 4b shows the projection of fast orientations.
Later the backazimuthal variation of fast orientations is modeled by means of two anisotropic layers.
Some stations (i.e. KBA, ARSA, OBKA) give Nulls in two groups of backazimuthal ranges, which can be related to either two fast orientations or single fast and single slow orientations.
We have shown that while the average values of fast orientations show clear mountain-parallel anisotropy pattern for the Western Alps, this pattern clearly breaks down in the Eastern Alps.
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