Transient rheology of the upper mantle beneath central Alaska inferred from the crustal velocity field following the 2002 Denali earthquake
The M7.9 2002 Denali earthquake, Alaska, is one of the largest strike‐slip earthquakes ever recorded. The postseismic GPS velocity field around the 300‐km‐long rupture is characterized by very rapid horizontal velocity up to ∼300 mm/yr for the first 0.1 years and slower but still elevated horizontal...
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Veröffentlicht in: | Journal of Geophysical Research: Solid Earth 2005-08, Vol.110 (B8), p.n/a |
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