晚期为脆性破裂构造，与早期变形组构具继承、叠加关系。
In the late period, brittle rupture structures inherited and were superimposed on the early deformation fabrics.
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。
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.
而且含金构造中岩石的组构特征、糜棱岩类型、应变幅度、石英变形机制与金矿富集程度都有密切的关系。
The gold abundance is also related to the type of mylonite, the feature of micro-fabric, the mechanism of quartz deformation and the size of strain.
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