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本文仅就北京西北延庆县张山营短水准所跨断层两盘的岩石热膨胀性的测量结果,讨论了该处的热形变特征,从而使消除热形变干扰后的短水准曲线中的地震异常幅度更加明显。
This paper only discusses the thermal deformation characteristics of the two sets of cross-fault rock mass near Zhangshanying short leveling station in Yanqing County, northwestern Beijing, so as to eliminate the thermal anomaly in the short-level curve after thermal deformation disturbance more obvious.