Convection Cells对流细胞
The early suggestion of plate tectonics were resisted because no mechanism for such plate movement could be found. Finally, in the 1930's, plausible models of plate movement based on convection cells were advanced. 板块构造理论的早期提出曾遭到抵制，因为尚无法找到解释此类板块运动的机制。直到20世纪30年代，基于对流细胞的板块运动 plausible 模型才被提出。
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Index References: Ward and Brownlee Ch 9 索引参考：Ward和Brownlee第9章 | ||
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Fluid Rock Behavior流体岩石行为
The suggestion of the continental drift associated with plate tectonics was resisted strongly from the standpoint of the apparent rigidity of the Earth's crust. But with the increased temperature and pressure associated with depth inside the Earth, the properties of rock change. 与板块构造相关的大陆漂移假说从地球 crust 的明显刚性角度遭到强烈反对。但随着地球内部温度和压力的增加，岩石的性质会发生变化。
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Index References: Ward and Brownlee Ch 9 索引参考：Ward和Brownlee第9章 | ||
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