Published In
Open Journal of Earthquake Research
Document Type
Article
Publication Date
2-17-2015
Subjects
Cascadia Subduction Zone -- Strains and stresses -- Measurement, Cascadia Subduction Zone -- Surveys, Global Positioning System, Continental margins -- North America
Abstract
Using continuously operating Global Positioning Stations in the Pacific Northwest of the United States, over 100 station-station baseline length changes were determined along seven West-East transects, two North-South transects and in three localized areas to determine both the average annual strains over the past several years, and the variation in strain over the central Cascadia convergent margin. The North-South transects (composed of multiple baselines) show shortening. Along West-East transects some baselines show shortening and others extension. The direction of the principle strains calculated for two areas 100 km from the deformation front are close to per-pendicular to the deformation front. The North-South strains are 10?8 a?1, which is an order-of-magnitude less than the West-East strains (10?7 a?1). Along several West-East transects, the magnitude of the strain increases away from the deformation front. All West-East transects showed a change in strain 250 km inland from deformation front.
DOI
10.4236/ojer.2015.41003
Persistent Identifier
http://archives.pdx.edu/ds/psu/17313
Citation Details
Cruikshank, K. and Peterson, C. (2015) Current State of Strain in the Central Cascadia Margin Derived from Changes in Distance between GPS Stations. Open Journal of Earthquake Research, 4, 23-36. doi: 10.4236/ojer.2015.41003.
Description
Copyright © 2015 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/
Open Access