Time-Variable Deformation in the New Madrid Seismic Zone
Eric Calais1 and
Seth Stein2
New geodetic measurements show that the New Madrid is currently
deforming too slowly, if at all, to account for large earthquakes
in the region over the past 5000 years. This result, together
with increasing evidence for temporal clustering and spatial
migration of earthquake sequences in continental interiors,
indicates that either tectonic loading rates or fault properties
vary over a few thousand years.
1 Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, IN 47906, USA.
2 Department of Earth and Planetary Sciences, Northwestern University, Evanston, IL 60208, USA.