Changes in seismic velocity and apparent attenuation due to isotropic and anisotropic scattering : results from physical modeling
Much work is presently being done concerning small scale heterogeneities in the earth's crust. These heterogeneities range from pores in sedimentary rocks up to fluctuations in the density and seismic constants of the earth's crust with scale lengths of kilometers. The ability to study and...
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| Language: | en_US |
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2012
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| Online Access: | http://hdl.handle.net/1957/29422 |