根据野外地质观察和第四系的断错，在青岛即墨温泉盆地发现第四纪以来活断层。
Based on field geological observation and the preserved Quaternary offset, the authors discovered active faults since Quaternary in Jimo hot spring basin.
甲子湾断层使这些阶地错断变形，系舟山-太行山断块隆起沿该断层产生翘起运动。
These terraces were offset and deformed by Jiazhiwan fault, along which the uplifted Xizhou-Taihang fault block was tilted.
无论是单一型断层崖还是复合型断层崖，通过断层崖的平均扩散年龄和初始错断时间，就能推断出它在某一时刻的具体形态。
It is feasible to infer the specific shape of a fault scarp with the help of its average diffusion age and origin time of the scarp.
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