A GPS estimate of relative motion between North and South America

GPS velocity data are used to estimate the Euler vector describing rigid body motion of North America relative to South America. Assuming the boundary between the North and South American plates is located near the Fifteen Twenty fracture zone in the equatorial Atlantic, the Euler vector predicts ex...

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Veröffentlicht in:Geophysical research letters 1997-03, Vol.24 (5), p.535-538
Hauptverfasser: Dixon, Timothy H., Mao, Ailin
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container_issue 5
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container_title Geophysical research letters
container_volume 24
creator Dixon, Timothy H.
Mao, Ailin
description GPS velocity data are used to estimate the Euler vector describing rigid body motion of North America relative to South America. Assuming the boundary between the North and South American plates is located near the Fifteen Twenty fracture zone in the equatorial Atlantic, the Euler vector predicts extension across the Royal Trough up to 1 mm/yr, and convergence across the Barracuda Ridge at about 2 mm/yr, in agreement with geological estimates averaged over tens of millions of years. Further west, convergence between North and South America at rates up to 8 mm/yr may contribute to deformation of the Caribbean plate along its southwest boundary with South America.
doi_str_mv 10.1029/97GL00284
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subjects Americas
Boundaries
Convergence
Earth sciences
Earth, ocean, space
Estimates
Exact sciences and technology
Fracture mechanics
Internal geophysics
Mathematical analysis
Rigid-body dynamics
Solid-earth geophysics, tectonophysics, gravimetry
Tectonics. Structural geology. Plate tectonics
Vectors (mathematics)
title A GPS estimate of relative motion between North and South America
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