THE PALEOZOIC STRATIGRAPHIC BREAKS IN NORTHEAST CHINA

In Northeast China, of Paleozoic, there is one stratigraphic break in the south part and three in the north part, i.e. Ordovician, latest Late Silurian-Early Devonian and late Early Carboniferous-Late Carboniferous. They correspond with the stages of Paleo-Asian Ocean tectonic domain, ended at Early Triassic. After the last break, the Paleozoic strata of the north and south started to develop synchronously.