This paper focus on the basic characteristics of Lebaquan-Gongpoquan epicontinental arc and the dynamic background for its formation in the contiguous area across Gansu, Xinjiang and Inner Mongolia.
文中着重讨论了勒巴泉—公婆泉陆缘弧的基本特征及形成的动力学背景。
This paper focus on the basic characteristics of Lebaquan-Gongpoquan epicontinental arc and the dynamic background for its formation in the contiguous area across Gansu, Xinjiang and Inner Mongolia.
文中着重讨论了勒巴泉—公婆泉陆缘弧的基本特征及形成的动力学背景。
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