地质全息论

Theory of geological holography.

以自然界中全息现象存在的普遍性为指导,以客观存在的地质现象为依据,从全息的角度来对地质现象进行分析,正式提出了地质全息理论,认为地质体形态、地质信息和地质活动的频率等其局部与整体之间具有相似性或对应性,而且这种"整体(全息系统)"和"局部(全息元)"是相对的,与实际大小无关。这三种全息分别称为地质形态全息、地质信息全息和地质时间全息。任何地质体都是地质历史中不同种类、不同级别的地质全息系统的先后和交互作用下的结果,因此在某种具体的地质对象研究中确定其主控全息系统及其级别就显得非常重要。地质全息理论可以为地质学相关研究提供一个全新的理论依据和参考手段。

Directed by the universality of the existence of the geological holographic phenomena in nature, and based on the geological phenomena existed objectively, the geological phenomena are analyzed from holographic viewpoint. Then, we proposed the theory of geological holography which considers that the relationshlp between the part and the whole in the aspects of geological morphology, geological information and geological activity frequency may be of similarity and correspondence, and moreover, the whole （holographic system） and the part （holographic node） are relative concepts and not related with actual size. These three kinds of geological holography phenomena are respectively called as geological morphology holography, geological information holography and geological time holography. Any geological body is the result of the interaction, with variable sorts and grade, of geological holographic systems in certain order. Therefore, the ascertaining of major holographic system and its grade is of high importance in the study of certain geological object. The theory of geological holography offers a new theoretical base and reference tools for the geological study.