摘要
@@Rifting in eastern Asia was repeatedly active in the zone extending from Lake Baikal to the Pacific coast during the Late Mesozoic and Cenozoic. This process was characterized by slightly different styles within orogenic belts, cratons, and continental margins. One can define two main (Late Mesozoic and Cenozoic) rifting stages, which are further subdivided into two or three episodes (northeastern China and Sakhalin).