Abstract

Lateral variations of seismic attenuation are investigated using data from a linear seismic array deployed across southern Taiwan. The attenuation parameter t* is obtained by fitting the amplitude spectra of P and S waves with a theoretical spectrum using an ω2 model. The observed t* data are then plotted against the travel time, back azimuth, and focal depth, respectively, to explore the spatial variations of t* for P and S waves. Significant lateral variations of seismic attenuation are found between the eastern mountainous and western plain areas of Taiwan. Large attenuation contrast with depth in the east indicates that an anomalously high-attenuation zone is located in a shallower area north of the array in southeastern Taiwan. A 2D raytracing method is applied to show that the probable depth of the anomalous zone is at about 15–20 km. This anomalous attenuation zone coincides with an area marked by low-P and low-S velocities as well as a total absence of seismicity. The area is also marked by other prominent manifestations of active collision between the Eurasian and Philippine Sea plates, for example, high mountain ranges, rapid uplift, and high heat flows.

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