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Continental Layer-Bound Tectonics $$$$ A New Model for the Origin and Evolution of Basin-mountain System and Orogen

机译:Continental Loard Teactonics $$$$一种新型号的盆地 - 山地系统和orogen的起源和演变模型

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The basin-mountain system and the thrust superimposed orogen evolving from the system are the two major tectonic types of continental crust mobile zones, which are products of the process of rotational, gravitational and thermal energies. The Earth is made up of spheres of different geomechanical properties. Although laterally nonuniform, they are controlled by their underlying weaklayers at different levels, thus forming layer-bound structures at corresponding levels. Among them, the continental layer bound structure is of multi-level character, of which the crustal movement is dominated in form by basin-mountain system and thrust superimposed orogen controlled by the middle crust plastic layer. The theory of continental layer-bound tectonics established by our study of the China regional tectonics from the global angle will become a new theoretical basis surpassed the plate tectonic theory for the study of continental geological problems.
机译:从系统演变的盆地山体系和推力叠加的造成的叠加是大陆地壳移动区的两个主要构造类型,是旋转,引力和热能过程的产品。 地球由不同地质力学性质的球体组成。 虽然横向不均匀,它们由其底层的弱层控制在不同的水平,从而形成在相应水平的层状结构。 其中,大陆层绑定结构是多级特征,其中地壳运动以盆地 - 山地系统以形式支配,并由中间地壳塑料层控制的推力叠加造型。 我们对全球角度的中国区域构造学习建立的大陆层压构造理论将成为一个新的理论基础,超过了大陆地质问题的板构造理论。

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