We use cookies to ensure that we give you the best experience on our website. You can change your cookie settings at any time. Otherwise, we'll assume you're OK to continue.

Durham University

Research & business

View Profile

Publication details

van Wijk, J., van Hunen, J. & Goes, S. (2008). Small-scale convection during continental rifting: Evidence from the Rio Grande rift. Geology 36(7): 575-578.

Author(s) from Durham


Recent seismic imaging across the Rio Grande rift, western United States, revealed unexpected
structures in the underlying mantle. Low seismic wave velocity anomalies below the Rio
Grande rift have been interpreted as being partially of melt origin, and high-velocity structures
below the western Great Plains have been proposed to be the result of small-scale convection,
i.e., cold downwelling lithospheric material with probably a compositional contribution. We perform
a dynamic test of these interpretations using a passive rift model for isochemical convection.
The models self-consistently produce a rift localized at approximately the right distance
from the border to the nearby thicker Great Plains lithosphere. With realistic upper mantle
rheologies, small-scale convection forms, aided by the lithospheric step. The resulting thermal
anomalies produce seismic low-velocity anomalies below the rift of amplitudes similar to those
imaged seismically, requiring the presence of only small amounts of melt. The lateral extent of
the observed low velocities below the Rio Grande rift is as in the models, where it is controlled by
the spacing between downwelling limbs of the small-scale convection. The fast velocity structure
below the western Great Plains can be produced by cold downwelling lithosphere. The thermal
rifting models can predict the amplitudes and size of the main seismic anomalies; compositional
heterogeneity may contribute to some of the smaller features observed.