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地壳层状构造特征在于坚硬层和软弱层互层性。地球物理探测表明,软弱层亦即塑性波导层可视为多裂缝、易渗透、饱含流体的地带,地壳是由多个软弱层构成的复杂多层体系。地壳波导层的动力学自振模型的提出,正是基于地壳的这种特殊的层状构造。该模型可以较好地解释地壳内矿床包括油气田的生成过程。认为完全可能存在两种不同的油气田成因,指出两种矿田的产生过程是同时、同地进行的。提出:“波导层本身一旦出现就会引起周期性朝上和朝下的垂直运移。这些运移必将冲洗沉积盖层,随之将烃析出。”也有观点认为,这种朝上朝下的运移活动是否同等发育或是否具有相同的规模还需进一步探讨。
The crustal layered structure is characterized by the interlamination of hard and weak layers. Geophysical exploration shows that the weak layer, that is, the plastic waveguide layer can be regarded as a multi-fractured, easily permeable and fluid-saturated zone. The crust is a complex multi-layer system composed of multiple layers of weakness. The proposed kinetic self-vibration model for the crustal waveguide layer is precisely based on this special crustal structure of the crust. The model can better explain the formation of the crustal deposits, including oil and gas fields. It is considered that there are totally two possible causes of oil and gas fields and it is pointed out that the production processes of the two ore fields are carried out simultaneously and in the same place. Proposed that “the waveguides themselves, if they occur, will cause periodic upward and downward periodic vertical migration, which will inevitably wash the sedimentary cover and subsequently separate the hydrocarbons.” It is also argued that this upward-downward Whether the same or not the same size migration development needs further exploration.