摘要
Linxi area between Siberian plate and Sino-Korean plate, located in the eastern part of Nei Mongol, is one of the most important regions for studying the paleo-suture between the plates. Up to now, there are two basically different viewpoints on the paleo-suture situation. Some geologists consider that the suture is situated oa the Xar Moron fault belt (almost in accord with the Xar Moron river valley); the others claim that the suture might be locat-
