Preliminary results of SKS splitting and teleseismic tomography suggest a lithospheric origin for Newberry. First, there is no asthenospheric anomaly beneath the Newberry, instead low anomaly is beneath all of the HLP. Second, no flow observed in asthenosphere along the track.
Berkeley Seismological Laboratory
215 McCone Hall, UC Berkeley, Berkeley, CA 94720-4760
Questions or comments? Send e-mail: email@example.com
© 2005, The Regents of the University of California