Miocene–Pleistocene deformation of the Saddle Mountains: Implications for seismic hazard in central Washington, USA

Author:

Staisch Lydia12,Kelsey Harvey3,Sherrod Brian2,Möller Andreas4,Paces James5,Blakely Richard1,Styron Richard67

Affiliation:

1. Geology, Minerals, Energy, and Geophysics Science Center, U.S. Geological Survey, Menlo Park, California 94025, USA

2. Earthquake Science Center, U.S. Geological Survey, University of Washington, Seattle, Washington 98195, USA

3. Department of Geology, Humboldt State University, Arcata, California 95521, USA

4. Department of Geology, University of Kansas, Lawrence, Kansas 66045, USA

5. Geoscience and Environmental Change Science Center, U.S. Geological Survey, Denver, Colorado 80225, USA

6. Earth Analysis, Seattle, Washington 98105, USA

7. Global Earthquake Model Foundation, Pavia 27100, Italy

Publisher

Geological Society of America

Subject

Geology

Reference97 articles.

1. Quantitative Seismology, Volume 1;Aki,2002

2. Inverse and forward numerical modeling of trishear fault-propagation folds;Allmendinger;Tectonics,1998

3. Estimation of fault propagation distance from fold shape;Allmendinger;Implications for earthquake hazard assessment: Geology,2000

4. Eruption chronology of the Columbia River Basalt Group;Barry,2013

5. Probabilistic Seismic Hazard Analyses Project for the Mid-Columbia Dams: Prepared for Public Utilities Districts of Chelan, Douglas, and Grant Counties;Benjamin and Associates, URS Corporation, Geomatrix Consultants, and Shannon & Wilson,2012

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