对现有假说的分析（Analysis of the existing hypothesis）.doc

对现有假说的分析（Analysis of the existing hypothesis） Analysis of the existing hypothesis of the seven principles of earth science Guangdong Marine university Yong-yan liao (E-mail: rock6783@126.com) Said inflation is based on evidence from earth, and weve listed above 60 generally accepted the fact that, at some point in their evolution of the earth, ocean did the rupture in the mid-ocean ridge, mid-ocean ridge magma upwelling caused by seafloor spreading; There are indeed rift valley on earth; Between the plates, there is also a phenomenon of separation. These basic facts are not to be denied. So, there is a volume of expansion in the earth at some stage in its evolution, or at some stage, or some phase. This is caused by the expansion of the earths volume. So, to some extent, the expansion of the earth is correct. Said the earth expansion of the earth, of course, the expansion of the volume of more than 1/10, and they have put forward the dynamic mechanism of the earth expansion, due to not strong evidence of positive support, and at the same time under a lot of evidence to the contrary in the negative, therefore, must be wrong. From the fact that the earth shrinks and says the evidence based on the facts, and the 60 of the facts that weve enumerated, its true that at some point in the evolution of the earth, there are indeed slots; Because it is accepted that the continental crust is formed by the ocean. The continental crust is highly wrinkled and metamorphic. The unwrinkled oceanic crust, which would become a highly wrinkled continental crust, must have experienced horizontal lateral pressure. The near circular basin is to become a linear geosyncline, and there must be horizontal lateral extrusion pressure. The earth also has a phenomenon of plate drift. Since there is a stage, a region, or a phase in the evolution of the earth, the unwrinkled oceanic crust becomes a highly wrinkled continental crust; The near round ocean basin is pressed to form a linear geosyncline;