Little late Holocene strain accumulation and release on the Aleutian megathrust below the Shumagin Islands, Alaska

Author:

Witter Robert C.1,Briggs Richard W.2,Engelhart Simon E.3,Gelfenbaum Guy4,Koehler Richard D.5,Barnhart William D.2

Affiliation:

1. Alaska Science Center; U.S. Geological Survey; Anchorage Alaska USA

2. Geologic Hazards Science Center; U.S. Geological Survey; Golden Colorado USA

3. Department of Geosciences; University of Rhode Island; Kingston Rhode Island USA

4. Pacific Coastal and Marine Science Center; U.S. Geological Survey; Santa Cruz California USA

5. State of Alaska, Division of Geological and Geophysical Surveys; Fairbanks Alaska USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference29 articles.

1. Beavan , J. 1994 Crustal deformation measurements in the Shumagin seismic gap, Alaska 195 205

2. Re-examination of the potential for great earthquakes along the Aleutian Island Arc with implications for tsunamis in Hawaii;Butler;Seismol. Res. Lett.,2012

3. Modern foraminifera, δ13C, and bulk geochemistry of central Oregon tidal marshes and their application in paleoseismology;Engelhart;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2013

4. The Shumagin Islands, Alaska, earthquake of 31 May 1917;Estabrook;Bull. Seismol. Soc. Am.,1992

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