รายละเอียดผลงาน

The first model of two layers is presented to study the anisotropy pattern beneath Myanmar and Thailand using shear-wave splittings. The measurements showed that a two-layer model beneath stations better explicates the splitting observations than a single-layer model. . Two groups of ???? can be classified and matched with West-Burma Terrane (WBT) and Shan-Thai Terrane (STT). The ???? represents that West-Burma Terrane moves in a northward direction, Shan-Thai Terrane and Indo-China Terrane (ICT) move in a south-eastern direction, and West-Burma Terrane has less anisotropy of ???? than Shan-Thai Terrane.