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Although the transition described here is more common, trench-perpendicular to trench-parallel transitions in φ have also been observed, for example, in Kamchatka and Alaska. These backward transitions are not easily explained by our model; however, because both Kamchatka and Alaska are located near slab edges, local processes may affect these regions
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Although the transition described here is more common, trench-perpendicular to trench-parallel transitions in φ have also been observed, for example, in Kamchatka and Alaska. These backward transitions are not easily explained by our model; however, because both Kamchatka and Alaska are located near slab edges, local processes may affect these regions.
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We thank the Alaska Regional Network, Alaska Tsunami Warning Seismic System, the Pacific Orient Seismic Digital Observation Network POSEIDON, and the Incorporated Research Institutions for Seismology/United States Geological Survey for providing data used in this study. We thank M. Behn and S. Pozgay for useful discussions and L. Wagner for assistance with figures
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We thank the Alaska Regional Network, Alaska Tsunami Warning Seismic System, the Pacific Orient Seismic Digital Observation Network (POSEIDON), and the Incorporated Research Institutions for Seismology/United States Geological Survey for providing data used in this study. We thank M. Behn and S. Pozgay for useful discussions and L. Wagner for assistance with figures.
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