鲜水河断裂带以强烈的现代地壳运动和频繁的地震活动而著称。在300余千米的长度上自1725年以来的250年间,已发掘的强震史料表明,6级以上的强烈地震已达20次之多。其中7级以上大震高达7次,平均每隔35年就有一次,强度之大,频度之高为当代少见。沿断裂带现代地壳运动的地貌形迹表明,它与土耳其北阿那托利亚断层和美国加 The Xianshuihe fault zone is known for its intense modern crustal movement and frequent seismic activity. During the 250 years since 1725 over a length of 300 km, the historical data of the strong earthquakes that have been excavated indicate that there have been as many as 20 strong earthquakes of magnitude 6 or higher. Among them, seven or more large earthquakes up to 7 times, an average of once every 35 years, the intensity of the high frequency of rare contemporary. The topography of the modern crustal movement along the fault zone shows that it is associated with the northern Anatolian fault of Turkey and the United States plus