断错水系 所谓断错水系指的是由于断层活动,主要是走滑错动造成穿过断层的河谷被错动变位,发生急剧转折以至水系重新配置的现象。它是判定活动断层的一个重要标志。是研究地壳水平运动,断层走滑活动状况的重要对象。利用断错水系所反映出的断层错动情况结合古地震的研究可作为判断断层位移速率、大震重复率的一个方法。在我国,对断错水系现象的注意 Broken water system The so-called broken water system is due to fault activity, mainly due to slippage slip caused by the fault of the valley was dislocation displacement, a sharp turning point and the water system to re-configure the phenomenon. It is an important indicator of active faults. It is an important object to study crustal horizontal movement and fault slippery activities. Using the fault dislocation reflected in faulty water system combined with the study of paleoseismic can be used as a method to judge the fault displacement rate and the earthquake repetition rate. In our country, pay attention to the phenomenon of water system fault