Abstract
Deformation within the North American plate in response to various tectonic processes is modeled using an elastic finite element analysis. A coarse grid contains 328 elements and 190 nodes, while a fine grid contains 718 elements and 396 nodes for a spatial resolution of 2°-3°. Information about the present-day state of intraplate stress constrains the modeling. Distributed ridge forces of magnitude 2×1012 N/m predict deviatoric stresses of the order of 20-40 MPa that are capable of accounting for the dominant observed ENE stress trend. Driving drag models also fit the trend but are not preferred because of a predicted tenfold increase in compressive stress magnitudes from east to west across the plate. -from Authors
Original language | English (US) |
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Pages (from-to) | 12,201-12,223 |
Journal | Journal of geophysical research |
Volume | 96 |
Issue number | B7 |
DOIs | |
State | Published - 1991 |
Externally published | Yes |
ASJC Scopus subject areas
- Condensed Matter Physics
- Physical and Theoretical Chemistry
- Polymers and Plastics
- Materials Chemistry