“…Mountains generally follows the northwest-southeast trend of the principal geological features: thrust faulting, with the fault planes perpendicular to the trend of the geological structures, is dominant, but considerable variance to the fault-plane orientations exists and strike-slip motion is not uncommon (Sobel et al, 1977c). In the Baikal rift zone, normal faulting is prevalent; Molnar, P., and P. Tapponnier, 1975.…”