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地质学报  2003 

中国西部盆山系统的耦合关系及其动力学模式――以龙门山造山带一川西前陆盆地系统为例

, PP. 177-186

Keywords: 盆山系统耦合关系龙门山造山带中国西部沉积盆地动力学模式C-型俯冲

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Abstract:

造山带与沉积盆地是形成于统一的地球动力学系统之中的一对孪生体,由此构造了盆山系统。盆山系统是陆块相互作用、岩石圈层圈相互耦合的复杂系统,主要表现为物质的循环系统和能量的交换系统。盆山系统形成演化过程中造山带和沉积盆地之间一切相互作用的总和即为盆山间的耦合关系。盆山系统是中国西部中新生代构造的基本格局,并有单测盆地型盆山系统和双测盆地型盆山系统两种基本类型。小陆块拼合、多旋回构造运动和陆内构造活动强烈等是中国西部盆山系统形成演化的地质背景。中国西部盆山系统盆山间耦合关系在垂向上表现为造山带隆升与沉积盆地沉降呈镜像关系,在横向上表现为物质流和能量流循环均有两个传递方向,并且盆山系统岩石圈各层圈间有着强烈的相互作用。中国西部盆山系统盆山间耦合关系的动力学模式为C(陆内)―型俯冲,对于单侧盆地型盆山系统其耦合关系的动力学模式为L(龙门山)―型俯冲,而双测盆地型盆山系统其耦合关系的动力学模式为T(天山)―型俯冲。

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