Abstract:
Tectonic stress regime in the Shillong plateau, northeast region of India, is examined by stress tensor
inversion. Some 97 reliable fault plane solutions are used for stress inversion by the Michael and Gauss
methods. Although an overall NNW-SSE compressional stress is observed in the area, the stress regime
varies from western part to eastern part of the plateau. The eastern part of the plateau is dominated by
NNE-SSW compression and the western part by NNW-SSE compression. The NNW-SSE compression in
the western part may be due to the tectonic loading induced by the Himalayan orogeny in the north, and
the NNE-SSW compression in the eastern part may be attributed to the influence of oblique convergence
of the Indian plate beneath the Indo-Burma ranges. Further, Gravitational Potential Energy (GPE) derived
stress also indicates a variation from west to east.