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Science 27 April 2001: Vol. 292. no. 5517, pp. 713 - 716 DOI: 10.1126/science.1058763
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Reports
A Complex Pattern of Mantle Flow in the Lau Backarc
Gideon P. Smith,1
Douglas A. Wiens,1
Karen M. Fischer,2
Leroy M. Dorman,3
Spahr C. Webb,4
John A. Hildebrand3
Shear-wave splitting analysis of local events recorded
on land and on the ocean floor in the Tonga arc and Lau backarc
indicate a complex pattern of azimuthal anisotropy that cannot be
explained by mantle flow coupled to the downgoing plate. These
observations suggest that the direction of mantle flow rotates from
convergence-parallel in the Fiji plateau to north-south beneath the Lau
basin and arc-parallel beneath the Tonga arc. These results correlate
with helium isotopes that map mantle flow of the Samoan plume into the
Lau basin through an opening tear in the Pacific plate.
1 Department of Earth and Planetary Sciences,
Washington University in St. Louis, 1 Brookings Drive, CB1169, St.
Louis, MO 63130, USA.
2 Department of Geological
Sciences, Box 1846, Brown University, Providence, RI 02912, USA.
3 Scripps Institution of Oceanography, University of
California, San Diego, La Jolla, CA 92093-0215, USA.
4 Lamont-Doherty Earth Observatory, Post Office Box
1000, 61 Route 9W, Palisades, NY 10964, USA.
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