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Articles
Crustal Structure of the Northeastern United States: Contrasts Between Grenville and Appalachian Provinces
1 Department of Earth and Planetary Science, Massachusetts Institute of Technology, Cambridge 02139
Average crustal models for the northeastern United States are computed on the basis of the travel times of P and S waves from regional earthquakes. The Precambrian Grenville Province in New York State has a relatively homogeneous crust. The Paleozoic New England Appalachians have a well-defined, two-layer crust that is slightly thicker and shows a high-velocity lower layer relative to the Grenville. A time-term analysis based on Pn data (waves refracted from the Moho) shows that a relatively thick or low-velocity crust parallels northeast-trending geologic structures in central New England. The observed differences between the two orogenic belts may reflect contrasts in their tectonic evolution. Revised on February 8, 1980
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Science. ISSN 0036-8075 (print), 1095-9203 (online)