Paleoearthquakes on the north Xizhou piedmont fault show that the switch from the last stable to the recent active tectonic stage was abrupt and intense.
从系舟山北麓断裂的古地震研究来看，从末次稳定期转入最新活跃期是突然的、强烈的。
Paleoearthquakes on the north Xizhou piedmont fault show that the switch from the last stable to the recent active tectonic stage was abrupt and intense.
从系舟山北麓断裂的古地震研究来看，从末次稳定期转入最新活跃期是突然的、强烈的。
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