A series of finite element models are used to simulate the evolving paleostress field within an accretionary prism during Late Cretaceous accretion in the eastern Aleutian arc-trench system,Alaska.
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释义
一系列有限单元模型模拟了阿留申岛弧板块边缘附加体在晚白垩世板块增生过程中古构造应力场的演变特征。
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