Sedimentary basin and adjacent orogenic belt are two basic tectonic units of continent and twins developed in a geodynamic system.

毗邻的沉积盆地与造山带是大陆构造的基本单元和形成于统一地球动力学系统中的一对孪生体。

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The rudimental guide of the plate-tectonic theory landing on continent is the archipelagic arc-basin system between the oceanic lithosphere and continental lithosphere.

大洋岩石圈与大陆岩石圈之间的多岛弧盆系构造域是板块构造登陆的入门向导。

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This basin developed numerous vertical migration pathways with good connectivity in fluids hold during tectonic activity, so the Junggar basin can be taken as a complex pool-forming dynamic system.

该盆地垂向通道众多，构造活动期流体上下连通性好，整体可划为一个复杂的成藏动力学系统。

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