东北亚陆缘晚白垩世从陆块碰撞到“安第斯型”俯冲的构造过程:来自中国东北白垩纪盆地构造-沉积演化的制约(英文)
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摘要
<正>A combination of the available stratigraphical,structural and sedimentary information from NE China defined a new tectonic process of NE Asian continental margin evolving from a continental block collision,through its departure to Andean-type subduction during the late Cretaceous.The Cretaceous basins in NE China can be subdivided into three NEN-trending groups,the eastern,central and western zones respectively.
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