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- W2016419005 abstract "Theories based on the assumption of an infinite medium show that the coda attenuation factor, Qc−1, of local earthquakes should be very close to the intrinsic Qi−1, whereas many observations show that Qc−1 is close to the total Q−(Qt−1). This paper shows by numerical modeling that Qc−1 depends on the thickness of the scattering layer. For source-receiver coincidence, if the thickness is greater than a half of the mean free path, Qc−1 lies between Qi−1 and Qt−1. However, when the thickness is less, Qc−1 may be higher than Qt−1. In addition, Qc−1 depends on the epicentral distance. The thinner the layer, the faster the change with distance in Qc−1. For an unbounded scattering medium Qc−1 is even lower than Qi−1 at long epicentral distances." @default.
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- W2016419005 date "1996-03-01" @default.
- W2016419005 modified "2023-09-27" @default.
- W2016419005 title "Effect of finite thickness of scattering layer on coda Q of local earthquakes" @default.
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- W2016419005 doi "https://doi.org/10.1016/0264-3707(95)00026-3" @default.
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