期刊
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
卷 106, 期 1, 页码 316-320出版社
SEISMOLOGICAL SOC AMER
DOI: 10.1785/0120150229
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This short note contains two contributions related to deriving depth-dependent velocity and density models for use in computing generic crustal amplifications. The first contribution is a method for interpolating two velocity profiles to obtain a third profile with a time-averaged velocity (V) over bar (Z) to depth Z that is equal to a specified value (e.g., for shear-wave velocity V-S, (V) over bar (S)(Z) = 760 m/s for Z = 30 m, in which the subscript S has been added to indicate that the average is for shear-wave velocities). The second contribution is a procedure for obtaining densities from V-S. The first contribution is used to extend and revise the Boore and Joyner (1997) generic rock V-S model, for which (V) over bar (S)(30 m) = 618 m/s, to a model with the more common (V) over bar (S)(30 m) = 760 m/s. This new model is then used with the densities from the second contribution to compute crustal amplifications for a generic site with (V) over bar (S)(30 m) = 760 m/s.
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