The continental margin of Northeast China and its adjacent areas is composed of two tectonic belts. The inner belt is a collage made up of fragments resulting from breakup of a palaeocontinent. The fragments are concerned with evolution of the palaeo-Asia
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唐克东 王莹.1995.中国东北及邻区大陆边缘构造[J].地质学报,69(1). Tang Kedong.1995. CONTINENTAL-MARGIN STRUCTURE OF NORTHEAST CHINA AND ITS ADJACENT AREAS[J]. Acta Geologica Sinica,69(1).
