A fault is not a simple plane, but a belt composed by a series of breaking planes or secondary faults, which is contradict with the hypothesis of the theory of cross-fault lithology juxtaposition.
断层一般不是一个简单的面,而是由一系列破裂面或次级断层组成的带,这与断层两盘岩性配置原理的假设有很大的差别。
We can use our achievement to rebuild some simple or complicated planes.
本课题的研究成果可用于简单或较复杂型面的逆向重构。
This paper advances a direct observational method to determine two principal planes corresponding with two principal stresses Belng simple and obvious, this method ean be mastered easily.
本文提出关于平面应力状态单元体上两个主平面与两个主应力对应关系的直观判断方法。
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