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本文对布设在著名的可可托海～二台断裂带上的三处三角观测场地和布设在额尔齐斯断裂带上的一处三角观测场地的三期观测资料进行了分析,提出了该断裂带当今的位移特征及构造应力特征,并对该区域构造活动的其它特性也做了有益的讨论。事实证明,该地区是大陆内部地壳活动剧烈的区域之一。通过对测量资料的仔细分析还可发现:在力源一定的条件下,由于断层各段走向的不同,同一断层各段所表现的张压特性可完全相反。
In this paper, three triangulated observatories located on the famous Keketuohai ~ Ertai fault zone and a triangular observational site on the Irtysh fault zone are analyzed, and the fault is proposed With today’s displacement characteristics and tectonic stress characteristics, and other characteristics of tectonic activities in the region also made a useful discussion. Facts have proved that the area is one of the areas where the continental crust activity is drastic. Through careful analysis of the measured data, it can also be found that under certain conditions of the force source, due to the different strike directions of the faults, the tension and compression characteristics of the sections of the same fault can be completely reversed.