Physics – Geophysics
Scientific paper
Jan 1995
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995georl..22..121l&link_type=abstract
Geophysical Research Letters (ISSN 0094-8276), vol. 22, no. 2, p. 121-124
Physics
Geophysics
7
Anisotropy, Boundaries, Chemical Composition, Earth Mantle, Earth Planetary Structure, New England (Us), Velocity, Anomalies, Geophysics, Seismology, Tomography
Scientific paper
Using teleseismic P wave tomography we detect very large (approx. 5%) variation in the compressional velocity of the upper mantle beneath the Proterozoic-Paleozoic boundary in the Northeastern US. In this region, the uppper mantle is heterogeneous on the 100 km scale to a depth of 300 km. Below this depth, the mantle appears to be laterally homogenous, at least on the scale of 200-250 km. Given the tectonic history of the region, the large amplitude, short wavelength heterogeneities cannot be caused by temperature variations, but may be due to chemical heterogeneity or variations in the amount and orientation of flow-induced seismic anisotropy.
Lerner-Lam Arthur
Levin Vadim
Menke William
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