Many normal faults with roughly the same strike and dip slide down from one side in turn, creating a stepped appearance in cross section. Source: About Shogakukan Digital Daijisen Information | Legend |
ほぼ同じ走向・傾斜をもつ多くの正断層が、一方から順にずり落ち、断面で見ると階段状を呈するもの。
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