提出了热流变构造诸如热流变断裂、热流变节理和热流变褶皱等新概念。
Some new concepts, thermorheological structure, thermorheological fracture, thermorheological joint and thermorheological fold etc.
它是在褶皱冲断带负载的作用下，岩石圈通过区域性均衡调整及流变挠曲而形成的。
They were formed through regional isostatic adjustment and Theological flexure under the load of fold-thrust belts.
因此，对褶皱的分形测量和岩层厚度及粘度的分析，可以定量分析分形褶皱形成的流变机理。
When buckling of a layer occurs during pure shear, the folds that develop are more complex and have bigger fractal dimensions with increasing thickness and viscosity of the folded layers.
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