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地质作用的阶段性与不可逆性
引用本文:冯乔,赵四海.地质作用的阶段性与不可逆性[J].西北大学学报,1997,27(4):340-344.
作者姓名:冯乔  赵四海
作者单位:西北大学地质学系(冯乔),科技干部进修学院(赵四海)
摘    要:从构造作用、生物演化、盆地形成等方面探讨了地球自形成以来所经历的各种复杂多变的地质作用。认为这种地质作用的形成与在地球漫长的地质历史发展过程中具有典型的阶段性与不可逆性;这种特性决定了地球在不同历史时期的构造作用机制、生物进化和盆地形成等都是不一样的,都具有旋回式递进变形的特征;地质作用的旋回式递进变形既可受控于内动力地质作用,也可来自于地球之外,但尚需做进一步研究。

关 键 词:阶段性  不可逆性  地质作用

The Phasic Property and Irreversibility of the Geological Functions
Feng Qiao,Zhao Sihai.The Phasic Property and Irreversibility of the Geological Functions[J].Journal of Northwest University(Natural Science Edition),1997,27(4):340-344.
Authors:Feng Qiao  Zhao Sihai
Institution:Feng Qiao 1) Zhao Sihai 2)
Abstract:The various and complicated geological functions, which the earth has undergone since it was formed, are discussed from the structural function, the organism evolution, the basin development and so on. It is suggested that their formation and development have the typical phasic property and irreversibility in the process of the very long geological history on the earth. They determined that the structural mechanism, the organism evolution and the basin formation could be very different, and have the cyclic characteristic of the progressive deformation to varing historial periods on the earth. The cyclic progressive deformation of geological funtions might be controlled by the internal power agency, and also might come beyond the earth, the mechanism of which must be further researched.
Keywords:phasic property  irreversibility  geological function  
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