Abstract
AbstractUsing the three‐components teleseismic records, we inverse the S‐wave velocity structure beneath the 59 teleseismic stations of Taiwan by the transform function method and the SA techniques. The integrated results show that the thickest part of the crust is at the western flank of Central Range. This conclusion is consistent with the result from the Bouguer gravity anomaly. The orogenic evolution of Taiwan is at the young period, and the foot developing of the Central Range is far from balance. The crust of Taiwan stays in the course of dynamic equilibrium.
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