fault fold zone 曾称断褶带
Tuositai reverse fault-fold zone 托斯台逆断裂
fault-related fold structure zone 断层相关褶皱构造带
Structural characteristics of inversion structure, fold association style, thrust fault zone upright strata developed belt shown in great profiles were also discussed.
对剖面中反映的构造反转、褶皱组合样式、逆冲断裂带、直立地层发育带的构造特征进行了探讨。
The structural style found in the basin includes imbricated thrust zone, trapdoor structure, drag fold, listric fault, rollover anticline, horst-graben structure and the like.
盆地中发育多种构造样式,主要有:叠瓦状冲断层、滚板构造、牵引褶皱、铲形正断层、滚动背斜、“垒一堑”构造等。
Moreover, the front of individual fold-reverse fault zone consists of several fault strands, which are associated with folds and have different ages of formation and time of recent activity.
除此之外,各排褶皱-逆断裂带前缘都由多条断裂组成,它们与褶皱伴生,具有不同的形成和新活动时代。
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