'Forebergs', flower structures, and the development of large intracontinental strike-slip faults: the Gurvan Bogd fault system in Mongolia

The Gurvan Bogd mountains of the Gobi-Altay, Mongolia contain a system of s trike-slip faults with a reverse component, part of which moved in a large earthquake (M(w)similar to 8.0) in 1957. Adjacent and sub-parallel to the m ain ranges are numerous thrust-related folds, thrust faults, and elongated low ridges ('forebergs'), all of which result from the shortening component on the fault zone. The appearance of these thrust-related structures is va ried, depending on their stage of development, preservation, and exposure. Evidence from geomorphology and surface ruptures suggests that they may all serve a common function, which is to broaden the deforming zone by creatin g new structures that are able to accommodate both the strike-slip and the shortening components of motion. The geomorphology further suggests that th ese new structures then evolve by lateral propagation and increase in ampli tude, to eventually merge and form through-going new faults subparallel to the old. In their early stages the new faults and related structures appear to be influenced by the underlying sediments adjacent to the main range, w hich may include weak layers such as lake beds that can ultimately cause th e collapse of foreberg ridges in landslides. The migration of faulting away from the main range is likely to be driven by stresses associated with top ography, which in turn is a consequence of the shortening component. The ev olution described here is thus peculiar to strike-slip faults with a revers e component, and can form many of the features of the 'flower structures' t hat are often described in such oblique-shortening zones. Although the shor tening component is often localized in restraining bends, its origin may ul timately be related to rotations about vertical axes, which are common in d eforming continental regions. (C) 1999 Elsevier Science Ltd. Ail rights res erved.