A fault is in 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.

• 摘要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。