In the late period, brittle rupture structures inherited and were superimposed on the early deformation fabrics.
晚期为脆性破裂构造，与早期变形组构具继承、叠加关系。
Hong, R. H. (1994) Analysis of deformation fabrics in the Sani thrust sheet and the Chuhuangkeng anticline of western Taiwan. Petroleum Geology of Taiwan, 29, 105-126.
洪日豪(1994)台湾西部三义逆冲断块及出磺坑背斜的变形组构分析。台湾石油地质，第29号，第105 - 126页。
The approach starts from an analysis of the weave pattern and finds out the basic deformation element of the woven fabrics: visible thread segment.
首先从分析编织式样的结构入手，得出编织式样变形的基本单元——可见丝线段；
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