fault-fold zone 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
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。
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。
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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