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Science 22 May 1998: Vol. 280. no. 5367, pp. 1245 - 1249 DOI: 10.1126/science.280.5367.1245
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Reports
Viscosity of Oceanic Asthenosphere Inferred from Remote Triggering of Earthquakes
Fred F. Pollitz,
Roland Bürgmann,
Barbara Romanowicz
A sequence of large interplate earthquakes from 1952 to 1965 along
the Aleutian arc and Kurile-Kamchatka trench released accumulated stresses along nearly the entire northern portion of the Pacific Plate
boundary. The postseismic stress evolution across the northern Pacific
and Arctic basins, calculated from a viscoelastic coupling model with
an asthenospheric viscosity of 5 × 1017 pascal
seconds, is consistent with triggering of oceanic intraplate earthquakes, temporal patterns in seismicity at remote plate
boundaries, and space-based geodetic measurements of anomalous velocity
over an area 7000 by 7000 kilometers square during the 30-year period after the sequence.
F. F. Pollitz and R. Bürgmann, Department of Geology,
University of California, Davis, Davis, CA 95616, USA.
B. Romanowicz, University of California Seismological Laboratory, 475 McCone Hall, Berkeley, CA 94720, USA.
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