The Origins of Mantle Anisotropy beneath Eastern North America
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The goals of this project were to better constrain variations in seismic anisotropy beneath eastern North America and to use the distribution of anisotropy to infer patterns of asthenospheric flow and lithospheric deformation. STS-2’s were deployed at four sites in southern New York (VASR, WIND, WICK, and SCCC) in June, 1997. The instruments at VASR and WIND were moved to UCON and UHRT (Connecticut) in October, 1998, and the experiment ended in February, 1999. Data was recorded continuously at 20 sps and 1 sps.
创建时间：
2015-07-13
